geophys rpt on the satterly prop satterly tp...the satterly property is located on birch lake in the...

52N08SW2001 2.18519 SATTERLY LAKE 010

Dan Patrie May, 1998

GEOPHYSICS REPORT

ON THE

SATTERLY PROPERTY

SATTERLY TOWNSHIP

RED LAKE

MINING DIVISION

FOR

EAST WEST RESOURCES LTD

AND

CANADIAN GOLDEN DRAGON LTD

JOINT VENTURE

BY

Dan Patrie

52N08SW2001 2.18519 SATTERLY LAKE 010C

TABLE OF CONTENTS

INTRODUCTION

SUMMARY AND RECOMMENDATIONS

PROPERTY LOCATION AND ACCESS

CLAIM DESCRIPTION

GEOLOGY

INSTRUMENTATION AND WORK DONE

INTERPRETATION

CONCLUSIONS

RECOMMENDED EXPLORATION PROGRAM

PERSONNEL

REFERENCES

CERTIFICATE OF QUALIFICATION

LETTER OF CONSENT

PSEUDOSECTIONS

PAGE

Page l

INTRODUCTION

East West Resources Ltd and Canadian Golden Dragon Ltd optioned a block of mining

claims from Perry English of Red Lake Ontario. It consists of 6 unpatented mining claims 75 units

located in Satterly Township, Red Lake Mining Division.

East West Resources Ltd and Canadian Golden Dragon Ltd requested Dan Patrie

Exploration Ltd., to do a limited exploration consisting of a geophysics program consisting of line

cutting and induced polarization survey. The survey began on May 13, 1998 to May 19 1998.

SUMMARY AND RECOMMENDATIONS

The Satterly Property is located in the Northern part of the Birch Lake area, Red Lake

Mining Division, Patricia Portion, District of Kenora, Ontario approximately 75 kilometers east of

Red Lake. Prospecting activity began in the area in 1926 and continiued through the 40s with the

main accent being on the search for economic gold mineralization.

The supra crustal rocks of the area are Archean (Early-Precambrian) in age and are from

2.9 to 2.7 b. y. old. These units which form the Birch-Uchi Lake metavolcanic belt, are enclosed

in an envelope of granitic rocks within the Uchi Subprovince of the Canadian shield.

Beakhouse (1985) indicates that the area has high potential for the discovery of base metal

massive sulphide and gold deposits. He considers the most favorable areas for base metal sulphide

deposits are the lenses of felsic metavolcanics, and the most favorable environments for gold

mineralization are; sheared zones associated with major faults and deformation zones particularly

where alteration veining and disseminated sulphides are present and areas within and marginal to

the fine grained high level felsic intrusions.

A total of 23.2 kilometers of induced polarization was surveyed. The survey indicated

areas of high chargeability anomalies which could host massive sulphides or precious metals.

Due to the lack of geological information, the following programs are recommended to

complete the evaluation.

1. Completion of grid lines over all of property.

2. Magnetometer and VLF survey on existing grid.

3. Completion of induced polarization survey over all of property.

4. Compiling past and present data for possible drill targets. #

Following the completion of this work and contingent upon the results, additional work

could be considered to further evaluate the property for gold and base metal mineralization.

The following report summarizes the results obtained from the work carried out during the

current exploration program and the interpretation is speculative.

Respectfully submitted,

Daniel F. Patrie

Geology and Geophysics Technologist

May, 1998

PageS

PROPERTY. LOCATION AND ACCESS

The Satterly property is located on Birch Lake in the central portion of Satterly township,

approximately 103 km (64 miles) east-northeast of Red Lake, Ontario, in the District of Kenora,

Patricia Portion, Red Lake Mining Division.

Float plane or helicopter, available in Red Lake provide access to the area.

Recently constructed logging roads from Ear Falls up the South Bay road provide access

in winter to approximately l hour by snow machine to the property.

CLAIM DESCRIPTION

*i

The property consists of 6 unpatented mining claims (62 units) situated in Satterly

Township, District of Kenora, Red Lake Mining Division.

TABLE l

SATTERLY PROPERTY. DISTRICT OF KENORA

RED LAKE MINING DISTRICT

CLAIM DESCRIPTION

MINING CLAIM EXPIRY DATE NUMBER OF UNITS

1215040 JUL 23, 1998 151215041 JUL 23, 1998 161215042 MAY,27, 1998 161215043 MAY, 27 1998 161215224 JUNE, 14,1998 12

Total 62 units.

MANITOBA

U.S.A

GENERAL LOCATION MAP

Z-K/V5 II64I49I l

r* TYT"tf

64147l 1118784 j

f —————-, -T

J2I0802.

64I20 15)04 2\S

IIG4I2ISour fi Bay

II64I26 I2I5043

64i 6

GEOLOGY

REGIONAL GEOLOGY

The area is underlain by Archean supra crustal rocks of the Birch-Confederation Lakes

Greenstone Belt in the western portion of the Uchi Subprovince. Preliminary mapping of the area

was undertaken by Thurston et al, (1981) who outlined a 1.5 km thick, east-trending sequence of

greenschist facies intermediate to felsic pyroclastic rocks with minor intercalated mafic

metavolcanic and metasedimentary rocks. This sequence is bounded to the north and south by

thick sequences of mafic metavolcanic rocks .

The area lies within the Birch-Uchi Greenstone belt which consists of north trending

volcanic and sedimentary rocks. The greenstone belt is 32 kilometers wide by 84 kilometers long.

INSTRUMENTATION AND WORK DONE

INDUCED POLARIZATION SURVEY

A total of 23.2 kilometers of induced polarization survey was done on the property with

readings taken every 50 meters and 6 levels l to 6 read except over areas where the lines were

short a 25 meter "a" spacing was used. The survey was a time domain pole dipole survey with a

"a" spacing of 50 meters and was read with a Walcer MG-2 motor generator and a Pheonix IPT-1

Model transmitter and a Scintrex IPR-12 receiver. The motor generator and transmitter were

stationary on the end of the line being read and current transmitted through a wire with an

PageS

electrode driven down through the ground for a good contact and then transmitting current to

that electrode from the transmitter by the transmitter man which is contact by radio to the receiver

man. Ahead of the live current electrode is a crew of men driving electrodes in winter and using

porous pots in summer at every station to be read and connected to the pots or electrode by

length of wire from the receiver where the receiver operator picks up the readings in the receiver

with the IPR-12. The data is then downloaded from the receiver at the end of the day to a

computer where the resistivity and chargeability is calculated and plotted using Geosoft software

for the earth sciences in pseudosection maps accompanying this report.

INTERPRETATION

The induced polarization survey detected anomalous areas on portions of the property.

Line 100W a zone at end of at 0+50N.

Line 2+50W 2 zones centered at 0+50N and 3+OOS.

Line 400w, a small zone at 0+50N.

Line 450w 2 zones, O to 200N and O to 300S.

Line 200W a zone centered at 400S.

Line 1200W a 200 meter wide zone centered at 0+50N.


Line 1800W a wide zone from O to 1000S.


Line 2400W parallel zones centered at O, SOON and SOON, and 400S.

Page?

RECOMMENDED EXPLORATION PROGRAM

The following program is recommended to evaluate the property for its potential to host a

precious metal and or base metal deposit.

1. Complete the line cutting as required to provide a control geological, geochemical

and geophysical work.

2. Geochemical sampling over target areas before drilling.

3. Magnetometer and VLF-EM survey.

4. Detailed Induced Polarization.

5. Geological mapping

6. Stripping, trenching and sampling over areas.

As a result of encouraging data obtained from the recently completed geophysics survey

additional exploration on the property is recommended.

Daniel F. PatrieGeology and Geophysical TechnologistMay, 1998

REFERENCES

1.Corfu, F., and Wallace, H., 1986,

U-Pb Ages for Magnetism in the Red Lake Greenstone Belt, Northwestern Ontario,

Canadian Journal of Earth Sciences, V.23, p27-42.

2. Horwood, H. C., 1940,

Geology and Mineral Deposits of The Red Lake Area, Ontario Department of Mines,

Annual Report, v.49, part 2, 23 Ip.

3. Hugon, H. and Schwerdner, W. M., 1084,

Structural Signature and Tectonic History of Gold Bearing Deformed Rocks in

Northwestern Ontario, p. 164-176 in Geoscience Research Grant Program, Summary

of Research, 1983-1984, Ontario Geological Survey, Misc. Paper 121, 252p.

4. Pirie, J., 1981

Regional Geological Setting in Gold Deposits in the Red Lake Area, Northwestern

Ontario, in the Genesis of Archean, Volcanic Hosted Gold Deposits, Ontario

Geological Survey Miscellaneous paper 97 p. 71-93.

PERSONNEL

Brent Patrie

P.O. Box 45

Massey, Ontario

POP 1PO

Serge Labelle

General Delivery

Walford, Ontario

POP2EO

Serge Masson

General Delivery

Sudbury, Ontario

Aaron Andress

General Delivery

Massey, Ontario

Micheal Burns

General Delivery

Massey, Ontario

Ron Bilton

Box 226

Massey, Ontario

CERTIFICATE OF QUALIFICATION

I, Daniel Patrie do hereby certify:

l . That I am a Geology and Geophysics Technologist and I reside at Hwy. 17 West, P.O.

Box 45, Massey, Ont, Canada, POP 1PO,

2. I graduated from Cambrian College Of Applied Arts and Technology, Sudbury, Ontario,

in 1987 with a diploma in Geological Technology with a one year certificate in

Geophysics,

3. And I have practiced my profession continuously since graduation, as well as being an

active prospector since 1972.

4. That my report on the Satterly property, Satterly Township, Red Lake Mining Division,

Ontario, is based on my personal knowledge of the geology of the area, and on a review of

published and unpublished information on the property and surrounding area.

Daniel F. Patrie

Geology and Geophysics Technologist (Dipl. T)

May, 1998

LETTER OF CONSENT

I, Daniel F. Patrie, of the Town of Massey, Ontario, do hereby consent to East West

Resources Ltd., and Canadian Golden Dragon Lid., using in whole or in part my Geophysics

report on the Satterly Property situated in Satterly Township, District of Kenora, Red Lake

Mining Division in a prospectus of statement of material facts or for filing with government

regulatory bodies as deemed necessary.

Dated at Massey, Ontario, this 27th day of May, 1998, in the District of Sudbury.

Daniel F. Patrie

Geology and Geophysics Technologist

998 89:45 7858442057

28 '98 88*53 FR GEOSCIENCE ASSESSMENT 7056705881 TO 917058442057 P.02^82

tSNfify •jJBnOa.iamiinii PlCljltfJOII Of ASTCsMMsrt^UinO a*** Performed en Mialif Laid

-^^ C

PROVINCIAL. *CCOHDIM*J

.S.O.

MAY 27

/J.

y of abaction* W121 and M(3) of ftbli e record. Tbi* inzonMtion will Tend hold*!. Questions "about thia Northern Development and Kin**, 3rd


- p*c wort performed on Czovn Land* before recording e clfqa, u*a fan 0240. fi**** *yp* os pcint in ink.

.ol (Attach m li*t if nece**ary)

fl DHXVIRT KBP LAJOr OHTARIO Telephone 801 727-21(7

IWft NuBfear 807 721-1117

OX 45 HASStt, CMTAJtXO, POP 1PO StiT.l.phona

t*S*ff-

work y*rfia A* e/- lfy"CoiSf*s' B. C.

: Ch*ck (/j uui xvport on only an of th* fallowing 9x019* foe tfci*

r It proBMotin*, surveys, rn fhyilcel: drilling etzipping, r"1 work w3*x tort ion H LJ trenching and aaaoeiateg^aasays LJ

MD IHOUCJD POLJUtlBATIOW

IS OS M

Day j Month J T.ar

To

19 OS tl

Day j Month J Toar

ling Syvtom Tovnihip/Acoa

IAKKoc -

OJfioo Uoo

Caaicdlty

MTS Rofocono*

Mining Division

KovldMt Coologla

c to-. - obtain a work permit from th* Minister of natural Xeaourcec a* required;- provide proper notice to oocfeee right* holder* before *t*jrting week;- ooM^lete and attach a Statement of Coat*, fort* 0212;- provide a ""P ehowing eontiguou* mining land* that are Linked for aaeigning wor)- include two eopiee of yous teehnxcel report.

who prapar*d th* t*dhNlOBl raport (Attach a list if n*c****ry)

W 1*0

Telephone NuMbcT* 144-2113709

Telephone HunfeeiT

-. d fey

IX, f.

HaldM- or Xgvnt

, do h*r*br that I h*v* pazvonal

2 7 1998

n Of JLmissaint Vbtk having caused th* work to b* perform** c i witnessed the saav during or to tha beat of my knowladga, tha anaavad rap* 11 li tiu*.

ox MWl 27/9*

i. t ••-'

* TOT AC

5. Work to b* recorded and distributed. Work can only be assigned to dal to the mining land where work was performed, at the time work was performed must accompany this form.

m that axe contiguous (adjoining) A map showing the contiguous link

Mialag dal* mfcer. Or if work was done on other eligible mining land, show in this column the location number indicated on the claim map.

*g

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2 '

3 '

4

5

6

7 '

8

9

10

11

12

13

14

15

TB 7827

1234567

1234568

1215040

1215041

1215042

1215224

1215043

1164158

1164159

Column Totals

oriMx of **i**^ Unit*. For other mining land, list

16 ha

12

2

15

16

16

12

16

4

4

i

75

Value of work performed on this claim or other mining land.

$26, 825

0

$ 8,892

$30 / 510.00 S

56,845. V '

$2,458.00 /

?2,370.00 '

0

0

$3,532 f

3FCOR

Value of workm?** toclaim.

N/A

524,000

5 4,000

56,000

56,400

56,400

54,800

56,400

51,600 '

0

V--

nPD ru A U i .. anno rc^Y 2 7 i nnH —

545, 715. X

i. . -j^FDSC

531,600

Value of work assigned to other mining claims .

blWM.Ot524,000

0

0

514,372

0

0

0

0

0

0

.JtZiVED-Y/ 2 7 ra3 ,) ̂ cteENCEASSESSMFN

1 i.-Mf'F"** - - - - - . ,-,

514,372

Bank. Value of work to be distributed at a future date

W(*l52,825

0

54,892

510, 138

5445.J4

0

0

0

0

53,532

|

.

517,275.^

DANIEL F. PATRIE er

do hereby certify that the above work credits are

subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the claimapp

where the work was done.

Signature of Rgeatded Holder^pr Agent Authorized in Writing DateMAY 27/98

6. Instructions for cutting back credits that are not approved.

Some of the credits claimed in this declaration may be cut back. Please check (/) in the boxes below to show how you wish to prioritize the deletion of credits:

X 1. ,Qredits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated.

D 2. Credits are to be cut back starting with the claims listed last, working backwards; or

Q 3. Credits are to be cut back equally over all claims listed in this declaration; or

(describe): 4. Credits are to be cut back as prioritized on the attached appendix or as follows

Note: If you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first,

followed by option number 2 if necessary.

For Office Use OnlyReceived Stamp

PROVINCIAL RECORDING OFFICE -SUDBURYRECEIVED

MAY 2 7 1998A.M, P.M.

Deemed Approved Date

Date Approved

Date Notification Sent

Total Value of Credit Approved

Approved for Recording by Mining Recorder (Signature)

Ontario Statement of Costs for Assessment Credit

TrOTRCtpVOJIMttmv (of 4i.ceWE C E l V E D

MAY271998VAtlB* A 'P'* PiM*

Personal information collected on this form is obtained under the authority of subsection 6 (1) of the Assessment Work Regulation 6/96. Under section 8 of the Mining Act, this information is a public record. This information will b* used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed to a Provincial Mining Recorder, Ministry of Northern Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury, Ontario, P3E 6B5.

Work Type

LINE CUTTING

INDUCED POLARIZATION

Units of work Depending on the type of work, list the number of hours/days worked, metres of drilling, kilometres of grid line, number of samples, etc.29.25

23.2

Associated Costs (e.g. supplies, mobilization and demobilization) .

2 TRUCKS, 6 MEN MASSEY TO RED LAKE AND RETURN

,G

MAY 2 7 19)Transportation Costs

AIR FLIGHTS

BOAT RENTAL

Food and Lodging Costs

Cost Per Unit of work

$325

$1,280

- , .-m ii ir" r\ ti.-i^ivbu jp:*l 21 I 'siW ;

3:6S6A \'OSCIENCE ASSfcSbMtwlj

fi?piHF

V 1 r^- 1-1.1

)ED38

Total Value of Assessment Work

Total Cost

$9,506.25

$29,696.00

$2,400.00

S3, 250. 66

9862.50

$45,^15.14

Calculations of Filing Discounts:

1. Work filed within two years of performance is claimed at 10(H of the above Total Value of Assessment Work.2. If work is filed after two years and up to five years after performance, it can only be claimed at of the Total

Value of Assessment Work. If this situation applies to your claims, use the calculation below:

TOTAL VALUE OF ASSESSMENT WORK x 0 .50 Total 9 value of worked claimed.

Note:- Work older than 5 years is not eligible for credit.- A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the Minister may reject all or part of the assessment work submitted.

Certification verifying costs:

I, Daniel F. Patrie- reasonably

do hereby certify, that the amounts shown are as accurate as may

(please print full name)be determined and the costs were incurred while conducting assessment work on the lands indicated on the accompanying

Declaration of Work form as certification.

I am authorized to make this

(recorded holder, agent, or state company position with signing authority)

Date

MAY 27/98

OntarioMinistry of Ministere duNorthern Development Developpement du Nordand Mines et des Mines

Geoscience Assessment Office 933 Ramsey Lake Road

August 25, 1998 6th FloorSudbury, Ontario

CROSS LAKE MINERALS LTD. P3E 6B5210-800 WEST RENDER ST.VANCOUVER, B.C. Telephone: (888) 415-9846V6C-2V6 Fax: (705) 670-5881

Visit our website at: www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm

Dear Sir or Madam: Submission Number: 2 .18519

Status Subject: Transaction Number(s): W9820.00061 Deemed Approval

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.

If you have any questions regarding this correspondence, please contact Lucille Jerome by e-mail at [email protected] or by telephone at (705) 670-5858.

Yours sincerely,

ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 12694

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2 .18519

Date Correspondence Sent: August 25, 1998 Assessor: Lucille Jerome

Transaction First Claim Number Number

W9820.00061 1215040

Section:14 Geophysical IP

Township(s) l Area(s)

SATTERLY

Status

Deemed Approval

Approval Date

August 25, 1998

Correspondence to:

Resident Geologist Red Lake, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):

Daniel PatrieMASSEY, ONTARIO, CANADA

CROSS LAKE MINERALS LTD. VANCOUVER, B.C.

PERRY VERN ENGLISH RED LAKE, Ontario

DANIEL F. PATRIE MASSEY, Ontario

Page: 1Correspondence ID: 12694

Casummit Lake .G 1 151

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S FOR STATUS REFER TO m? PLAN' No.

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RE FE RENCES

AREAS WITHDRAWN FROM DISPOSITION

M.R.O.-MINING RIGHTS ONLY

S.R.O. -SURFACE RIGHTS ONLY

M.+ S. - MINING AND SURFACE RIGHTS

Dweriptton Orctar No. DM* Dtvodtian FB.

LEGEND

HIGHWAY AND ROUTE No. OTHER ROADS TRAILS SURVEYED LINES:

TOWNSHIPS, BASE LINES, ETC.LOTS, MINING CLAIMS, PARCELS, ETC.

UNSURVEYED LINES:LOT LINESPARCEL BOUNDARYMINING CLAIMS ETC.

RAILWAY AND RIGHT OF WAY f UTILITY LINES NON-PERENNIAL STREAM FLOODING OR FLOODING RIGHTS SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINESTRAVERSE MONUMENT REMOTE TOURISM SITE (Rri)

DisrasmoN OF CROWN LANDSTYPE Of DOCUMENT SYMBOL

PATENT, SURFACE ft MINING RIGHTS..__............ 0" , SURf ACE RIGHTS ONiY......,...^,.......^.

" , MINING RIGHTS ONLY ___................^ OLEASE, SURFACE ft MINING RIGHTS..................... H

" .SURFACE RIGHTS ONLY._........,.^....... B" .MINING RIGHTS ONLY ..,...........-^ri^....... Q

LICENCE OF OCCUPATION ..__.....,.........M....-. T

ORDER-IN-COUNCIL ......... ...............,........... QC

RESERVATION ____....__............_...,. _ (J)

CANCELLED ____.....___. .,......... .... SAND ft GRAVEL .._...,___ - ,................. (*)

MOTI: MINma BIGHT* IN PAKCELS PATENTED PRIOB TO MAY 6 1*1*. VMTEO IN OMIQINAL PATENTEE BY TM6 PUBLIC LAND* ACT. m .t.O. 1 170. CHAP. MO. SEC. 63, SUBSEC 1.

SCALE: 1 INCH - 40 CHAINS

FEETp lOpO MOO

O 2OO ' 1OOO METRES ' (1 KM) •O 61998

"PROVINCIAL HkCUHuiiiOFFICE - SUDBURY

AREA

SATTERLY LAKEM.N.R. ADMINISTRATIVE DISTRICT

RED LAKE/ SIOUX LOOKOUTMINING DIVISION '

RED LAKELAND TITLES/ REGISTRY DIVISION

KENORA/PATRICIA

Ministryof LandNatural Management

Resources BranchOntario

OiUFEBRUARY 15, 1983

Ntmbtr

G-1874

THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES. AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON


1641561118717

1210802

BIRCH LAKE

EXIT BAY

1215224

1164120

1215042

1 164158

1215043

Om 200 400 600 800m

SCALE


DAN PAIR l E EXPLOATIONS LTD

EAST WEST RESOURCES Se CANADIAN GOLDEN DRAGON

JOINT VENTURESATTERLY CLAIMS

MAY 1998.

DRAWN BY KIMBERLY ZARICHNEY

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0=2 0.38 0.33 0.27 0.25 0.22 0.080 0.070 0.060 0.070 11=2

0=3 0.050 0.21 0.19 O.I! 0.18 0.20 0.10 0.080 0.050 11=3

n-4 S.060 0.030 0.15 0.15 0.17 0.14 0.19 0.12 0.070 n-4

P*s jsti"irw "50 N 2*00 N ^ 2*50 N JtOO N , 3*50 N f RssistivityOhm-m Filter TO 2315 1813 1334 1444 1899 2S8 304J 4740 3951 3372 Filter Ohm-m

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* * * * . V ' "* '""*- i l ' " - p lot pgint

JGEOSCiLf,.

Logarithmic , . ^ K Contours '- 1' 5 ' 2 ' 3 ' 5- 7' 5 ' l 0 '"

INTERPRETATION

* Strong increase in polarization accompanied by marked decrease in resistivity.

D Well defined increase in polarization without marked resistivity decrease.

O Poorlv defined polarization increase with ho resistivity signature .

T Low- r6Sjis^ivity feature .

Scale 1:250025 0 25 SO 75 10O 125 150

(metres)

ST RESOURCES/CANADIAN GOLDEN RESOU ? INDUCED POLARIZATION SURVEY

SATTERLY CLAIMS SATTERLY LAKE AREA

Date: 98/05/20 Interpretation: D.PATRIE

DAN PATPIE EXPLORATION LTD.Software ror me t ^

o mCN

l

5eao K

FM RES 1.6., 561 4.8.,

0.78. 280 l 2.4.

Metal Factor

Resistivity Ohm-m

Chargeability mv/v

-J——l——l——U

RES FM 561 r1.6

.2.4 '280

Filter 0.7! D.80 D.99 0.87 0.95 0.8! 0.8*

n=] 1 .6 Q.BO 1.Z 0.81 0 .50 0 -75 0 .87 1 .1 0.74 O.M 1 .1 1

n-2 1.2 M 1 O.Bt 0.43 0 .44 0.16 0 .60 0 ,65 O .H O W 0.98 1

0=3 3 72 C 87 1 .5 0 .99 1 I.Z O 49 t.J 0.54 0.64 O SO 0 .7? 1.2

0=4 5 .15 O 75 0 .34 O .SS t 0.09 0 .83 1 ,9 0.61 0.5E 0.68 0 .41 0.44 0 .83

0=5 1-1 0 .47 1 5 0.77 0.73 0 .97 0.66 1.4 0 .77

na6 0.8D 0.64 0.85 0.57 0.75 0.76 0.77 0.94 0 .80 1,2 0.60 0.40 O 33

1.2 14 1.3 1.1

1.1 1 071 l J

9.90 092 O.SS 0.80 0.43 O.SI 0.48 0.46 0.40 O.Z1

1.98 0.99 -0.80 t.4 0.21 0.88 0.73 0.39 0.18 0.020

0.90 /Ts\ 0.39 0.51 0.82 1.7 1.1 0.44 0.17 0.31 0.26 O.M O

2.1 ——1.9 090 0.14 0.84 1 0.17 0.53 0.40 0.36 0.49 0.33

0.45 056 060 0.55 1.8.—— 1.9 1.1 19

.47 I.! 2.i ' 1 .6 1.8

0.89 3.31 0.92 0.91 0 .21 0.22 0.4T 0.51 0.18

O.GB 1.S O.B3 0,23 0.31 0.72 O.SI G.*3

0.99 1.4 O.Bt 0.59 0.26 0.82 C W 0.41

n-2

n-3

n-5

n-6

510 439 40J 407 194 J21 334 M 341 331 330 322 510 354 372 386 404 4ZO 4M 430 426 408 391 354 p;|ter

187 1 91 ^ 162 171 1*1 ——— 140 150

235 31? —- 279^ 251 287 m

353 3* 335 J99 90 394 .MB 42! 406m '*~~~ 104 m 365 J20

44j wj 368 51* —— W 9) ve 350 368 330 327 *04 425 413 J HTx" 366 3S7 366 407 M^^- ̂ ——" ^ ——- 47t___47D __ *^ ̂ /^*9

544 53 ~~ 508 ^^^ 450 j SS8 546 -—- 494 ——— W ^*33 4J1 417 *OI 496 """^ 2B7 -^ 416 j^^MT"^ 444 444/531 SJB 633 616 576 (27 564

12 ' 581 ^ ,'4S 5W 488 ——— 476 501 475 (80 706 737 94 7 14 694H2 5(8 521 '2! [42 559 596 509-480

2.8 J.3 3.8 4,4 4.2 3.9 3.4 3.4 2.6 2.9 2.2 2.1 2 I.! 0.92 Finer39 3.4 J.5 3.5 3.6 3.3 3.2 3.2 2.8 2.

0=6 5.7 J.9 -^"5.1 — 3.3 3.9 5.6 *.9 5.J l.B

Metal Factor

Resistivity Ohm-m

Chargeability mv/v

Line O

Pole-Dipole Array

Filter*

* *

a = 50.0 M

r,. , pfot point l

?:SMtMT

Logarithmic, . s ? , . , , Contours '' '' 5 ' A J' b' 7' 3 '

INTERPRETATION

* Strong increase in polarizationaccompanied by marked decrease in resistivity.

D Well defined increase in polarization without marked resistivity decrease .

D Poorly defined polarization increase with no resistivity signature.

T Low resistivity feature.

Scale 1:500050 100 150 200 250 300

(metres)

EAST WEST/CANADIAN GOLDEN DRAGON J INDUCED POLARIZATION SURVEY



DAN PATRIE EXPLORATION LTD.Gevsbft Software 'or :re Earth Sciences

0

CN

H

X

B W E-i H

g

ey* HU) CO rH

CN

H O O

a003

^ O

FM RES XM XM RES FMQ 21 "HO."! 4 fi 4 K 94P.1 n ? Q

0.14, 4746. 2.

O-I 0-

Metal Factor Filter

0=1

0=2

0=3

0=4

Resistivity Ohm-m F lter

0=1

0=2

0=3

mV/V F iiter

0=1

0=2

0=3

0=4

3. \ .̂-S . .2.3 L4746 .0.14

s*'*' '

n i i i i i , r i , , i , , , r , , n In n

ItOON | 1+50 N ( 2*00 N r | 2+50 N i WON Mptnl Fnrtnr0.26 0.24 0.24 0.18 0.090 0.070 0.050 0.040 0.060 0.070 Filter

0.17 0.10 0.19 0.24 0.11 0.090 0.040 0.030 0.060 n-1

0.13 0.32 0.14 0090 0.080 0.070 0.030 0.050 Q. 040 0 = 2

0.49 0.29 0.070 0.070 0.060 0.050 0.050 0.030 D.D70 0=3

0.57 0.16 0.070 0.050 0.050 0.080 0.040 0070 0,25 0=4

ItOON 1+50 N 2+00 N 2+50 N 3+00 N Resistivity

2 95 2318 2219 2871 4260 5002 7380 8630 557C 6046 Filter Ohm-m

25J4 3686 ^2112^- ^292 2950 3840 x 8348 12K -, 4S46 0 = 1

89?' ' 1212 j 4985 44*6 5229 8142 -" 5747 ( 9277 J ̂ 3794 0=3

706' 2457 5068 6226 -8242 SsST"-' 7511 '"'4J6o' 1515 0 = 4

4.2 4 3.8 1.4 -'.3 3.4 3.4 3.3 2.9 2.9 Filter mV/V

4.3^ 3J __ ̂ 4 3.2 3.1 3.4 3.2 32 2.8 n-1 FA^T \

4 4.1 3.1 3.4 3.1 3.5 3.5 2.6 2.8 0 = 2

4.4 ^ 3.5 3.5 3.2 3.1 4~l 3 3 2.5 0 = 3

4 39 3.5 3.2 3.9 3.2 2.9 2.9 3.8 0=4

Line 200 W

Pole-Dipole Arraya no a

4 — (D-i r®-\Filtftr i 1 1

* N x , '

t \\ S \^ / ' 0 = 25.01^

t * *' * ~v' plot point

INTERPRETATION" Strong increase in polarization

accompanied by marked decrease in resistivity.


d Poorly defined polarization increase with no resistivity signature.

T Low resistivity feature .

Scale 1:250025 0 25 50 75 100 125 150

i i(metres)

EST RESOURCES/CANADIAN GOLDEN RESOUINDUCED POLARIZATION SURVEY


Date: 98/05/20 Interpretation: D.PATR1E

DAN PATRIE EXPLORATION LTD.Geosoft Software for the Eartti Sciences

FM RES XM 22, 24K 4*-,

11 j 12KJ

Oj Qj QJ

METAL FACTOR

o in

RES STIVITYOhrr-m

inCO

o o

x—KM RES FM .44 24K r22

D t! 0.20 J7 8.8 0.52

92 4.1— 7.7

n-2 1.45 0.080 3.060 O KC 3040

D,040 0.080 0.030 s~- 1 1//tf?o-rtK

0.27 O.IS 0.39 0.14 0.3 O 11

0.34 Q.45 3.67 2.2 l 5

0.47 O.J4 O.S6 i 75 O.M

.030 0.77 0.16 O 14 0.27 O.M C.91 O.tt 0.55 0.11

^fe^-

0.73 0.16 3.12 0.070 0.030

1.} 0.33 0.19 0.040 0.030

1 0.080 C.OK Q.(BO 0.050 0.030

O.C70 0.070 0.060 O 10 O.OBO O.OW

Flier

*0!^^-- 2* ;- 'M ^ "

. 321 •f f̂ 1 71 ^T M .— n jff'^ ~ 2**

—— '43 ra*^ 34^^1874 -^SW^-

-4.9 1.3-\ v./"

5l'-"V42 ——— *1 X/ 31 ' 24 l 15 14^ '7.8 y

W "^-"y" 'JO Z* y 14 ' 22 ——-IT^- 12

'2 9.5

" r'8,3 8.5 9.: 3.7

-92 S.fi 8.6 7 9.8 fl.B

S.1 fi.* B.7 9.1

M 88 9 .t 9 .1 x- 'O 7.5 7.7 9.1i l M 88 a.6 9.1 v- 1 0 7 5 7.7

' 13 'lO 8.4 10 11 ' 7 .8 9.4 'O'

1=3

METAL FACTOR

RESISTIVITY Ohm-m

CHARGABIUTY

Line 250 W

Pole-Dipole Array

———S^T t J -'f^1; initer i a \l y t- . b i_. w l V S^/tJ' jl*i * *

* * * * *

Loganthmic Contours 1, 1.5, 2. 3. 5, 7.5. 10...

INTERPRETATIONB Strong i ncrease in polarization

accompanied by marked decreasein resistivity.

D Wei! defined inc^ase in polarization without marked resistivity decrease.

d Poorly defined p olarization increase with no resistivity signature.

T Low resistivity feature ,

Scale 1:250025 O 25 SO 75 100 125 150

(metres)




____DAN PATKIE EXPLORATION

o vo

3H

Sea

mrt

ogD]

FM RES XM 0.25. 8720., 8.3

10.13. 4360.) 4.1.

0. oj 0.

Metal FactorFilter

0=1 C

n=2

0=3

0=4

Ohm-m Filter ~

0=1 3

0=2

0=3

.1=4

mV/V Fiiter

0-1

0=2

0=3

0-4

r5^c^v^--'x''X""x. -- N ^~""— --~I \ ^S? \

f " *"~'' \ —— ~~~

0+50 N 1+00 N 1+50 N 2+00 N 2+50 N J+00 N

.23 0.19 0.13 0.10 0.060 0.080 0.040 0.080 0.17 0.14 0.19 0.22 0.070

.19 0.13 0.060 0.070 0.040 0.010 0.080 0.040 0.27 0.34 0.34 0.52

0.26 0.1! 0.070 0.050 0.050 0.050 0.050 0.25 0.24 0.15 0.25 0.12

0.23 0.22 0.060 0.070 0.040 0.040 0.37 0.24 0.11 0.14 0.090 0.030

0.30 0.16 0.10 0.060 0.040 0.46 -0.96 0.12 0.16 0.060 0.020 0.05

335 3428 6037 5930 7927 6466 6261 4830 1547 1922 3150 4053 7162

441 3352 ?2*/ S568 - 9 I56 ^ — 4646 6848 s 1 045 ^—901 934 , 547

2980 3657 -- 6347 ' 8892 ' 5611 7932 — 6963 V;973^ 1407 -~ 2I19N JJM^ 2413

3910 f 2983 , 5J5^ 506' f "* ""'*// l036 l 4311 309I) 2IH ~~ 36S8 ^^" '*

2858 4692 — 4240 ' 8452 I2K'/ 1173 149! 3076 2652 4005 "^ 19Ki 5632

.5 6.6 6.3 4.8 4.2 3.4 2.8 2.3 2.3 2.2 3.3 3.1 3.2

.6^4.5 5.9 3.7 3.9 1.8 3.6 2.9 2.8 3.1 3.2 2.8

1.6 Te\ 4.7 4 2.6 3.8 3.5 2.4 3.3 3.2 2.9 3

9J\ 6.6"\5.l \ 3.6 s- 4 .;T~\v3.a —— (3.8 —— 3.4 3.3 2.9 3.1 3.5

8.5 •*- 7.4 ' 4.2 4.7 4.4 5.4^ -H 3.8 —— '4.3 3.3 3.5 2.!

XM RES FM p8.3 r8720 .0.25

\

.4.1 (.4360 .0.13

\

.0 Lo o

Metal FactorFilter

n-1

(1=2 0=3

0 n-4

Resistivity ™er Ohm-m

0=2

0=3

0=4

ChargeabilityFilter mV/V

0=1 EAST Vn=2

0=3

0=4

Line 400 W


' —— (EH r-®-] Filter i i 1

*

X \^ y ' a - 25.0 M

* * * * tf"

plot point

""':7'I^ 1

^

cOydnttlrfiic ^ i ^ ?* 7 c ^jz-c,— -th

INTERPRETATION* Strong increase in polarization


n Well defined increase in polarization without marked resistivity decrease.

d Poorly defined polarization increase with no resistivity signature .


Scale 1:250025 0 25 50 75 100 125 150

(metres)




DAN PATRIE EXPLORATION LW..-eosoft Software for the Earth Sciences

FM RES XM XM RES FM \

j ~-^ — sf\ s"^"\ ^ ™ ̂ i V'2. 25KJ 20. l \ S \ s**'*^ ^-. —— ——— --""""--^^^ .20 U25K .12 \*.

1 \X-^ ^X , ^^-^--"" l r

METAL FACTOR **005 3*5CS 3+OOS 2+HS 2+CQS 1+505 '+OOS 0*50S ( 0-00 D*50N t+OON U50N Z+OQ N 2+50N 3+OON MFTAL FACTOR

n-3 '2 ~—- 8.3 o 1 iTJBfO 1.3 0.040 0.020 O.Offi 0 0100 0 030 0.030 0.1* 0.96 0 26 Q. B Z 0.70 0 19 0.41 0.29 0.15 0.17 0,14 0.070 0.030 0.030 D. 040 0.030 n-3

1

RF^ iSTIViTY **B S JtSC 5 3*00 S Z+50 S 2+00 S 1+50 S 1*00 S 0+50 S 0+00 j 0*50 N 1*00 N 1+50 N 2+00 N 2*50 N 3+00 N Rp^TJVITY

Qhrn-Tl F" lter W ^ 4" ^ 3B3 S53 11K 24K 3* 41R 4(K 39* ZW 12K 4IU 4Z93 WE 5291 4530 8052 9S74 3388 73T6 6743 9236 W 14K I7K 19( 1* FiHer Ohm- m

0=1 531 - 44S *40 -^J8D __ 232 -^598 ,\vv ZOt i J7K 52K -^4* 57K 4* • W.^\îti 20^,^.68} —— 14M x BW^- 3K2 - K96 x 1EK /-x, 2ffi5 ^, 5554 3BT SW 51S7 5428 __ 13K x. 21K 0=1

^1=2 '22 476 4B7 3^^, W^jî^âK ̂ ^ÔK ^~ 51K -^5* m WK N' :^//- OT1 2185^T~*741 -1 390? -~J™ \ " ' 0 ( \*A ®* S 8512 94N 4212 7*7 — !757 y **} , 1*0" 2* 1=2

0=4 '!7 ' ' 377^ —— **J -* 747 10H "2187 ^* 13K ^- 22K '33K - UK i*^' W5* ^ 2360 ^' UK 12K ' 1BW J705 5048 — Z7M 6758 7747 - 6947 B077 ' 13K '^•*' 2W 17K 16K ~ 1W 17K 1=4

OARGAE'LiTY **00 S J+5C S XB S 2+50 S Z*CO S 1+50 S 1+00 S O5Q S CK)0 0+50 N 1+00 N 1+50 N 2OO N 2+50 N 3+00 N CHARC,ARI| ITYm ,j f-\i F iter J' M 15 26 M 27 '4 B.B 6.6 5.9 B.' 5.3 E 4 19 20 24 24 M '9 22 IB 15 IS 11 7,9 6. S 6 5.5 6 7.4 Fiiter mV/V

1=3 J3 , 3 S S /^ 26 SI^ 27 S 17 /^X 7.7 5.4 5.6 5 8 7-9 ~: * 7 5 V/ 24 23 24 24 1Z 22 /^ !9 20 l* 11 y 7.8 7.5 7.4 i*-^- 5' ! 9 ns3

V*^-* "" *-- VA^H^X ' f fm* iXn AAP

--•.f . LlllC rO^jL-^TT^^ P \rv'- " ,^-^^

^-^1^*D^^ Pole-Dipole A TO ya no o

* ——— ®-I r-lSH Rlfer 1 1 1

*V, v^ v' x a " 25 - 0 M* * * * ^ tf

plot poinr

ffiTl.1.5.2.3. 5.7.5. 10...

INTERPRETATION


D Well defined increase ir polarization without marked resistiv.ty cecrease.

D Poorly defined polarization increase with no resistivity siqna:jê.


Scale 1:250025 0 25 50 75 100 :25 1 50

(metres)


SATTERLY CLAIMSSATTERLY LAKE AREA

Date: 98/05/21 Interpretation: D. PATr ! E

DAN PATRIE EXPLORATION

oCO M

J xat W EH EH

HCN

FM RES XM XM RES FM n nss , 1 1 K s 7 * 7 1 1 K r) , "f"

i A v s*' ""*- ri \ \ ' i0.044. 5277' 2.9- \ _____ N""*~---j*-*;— -~^~--— ̂ ^~- ————— - -2 ' 9 t-5277 -0-044

y^tnl Fnr.tnr , \ *f)U 1 +50 N , 2+00 N ( 2+50 N , , 3rtO N , . J.50 N , M P tn| Fa^tnrniter 0.070 0.070 0.040 0.030 0.0*0 0.040 0.060 0.070 0.070 0.080 0.080 0.070 0.050 Filter

0=1 0.06C 0.030 0.050 0.080 0.060 0.090 O.I2 0.090 0.070 0.080 0.070 0.080 n-1

n~2 0 .050 010 0.020 0.040 0.060 0.050 0.080 0.070 0.090 0.080 0.070 0.040 (1=2

0=3 0.060 0.050 O.OaO 0.020 0.030 0.060 0.040 0.040 0.060 0.090 0.070 0.050 0=3

0=4 0.14 0.070 ) 040 0.060 -0.10 0.030 0.050 O.OJO 0.040 C. 070 0.10 0.060 n-4

Rp^tivity HMN 1+50 N 2*00 N 2+50 N 3*00 N 3+50 N R^ktivl+yOhm-m Filter 8802 '995 8500 9595 7027 5370 *908 5192 "465 3618 3765 4473 4M9 Filter Ohm-m

n-1 7959 6557 — 6846 3408 4098 2888 — 2595 ^ 2216 2481 3243 3921 3770 n-1! -^~~-N\ s'/ - ^\ O 1 s ——

0=2 "K \ 4391 l 10K 9995 x 3540 — 2867 5305 5077 N | 9II v 2712 4280 ' 6266 n=2J \ 1 1 N\\V ^ 1 f — x\ X^ \ i

0=3 9445 8849 -^ mg \ I 3K lin A x 2347 4047 1 9539 5897 x 2069 3463 6507 (1=3

n-4 3603 ~^"7454 ''in 8931 14K IOK -^ 3162 5908 1* 6881 2470^ 4118 (1=4

-hnrq^nhil+y , \ ™* "50 N i 2*00 N | 2+50 N 3+00 N 3+50 N ] Ohnrgpnhility

^yyy Filter 5.2 5.; 2.6 2.6 1.9 1.2 2.5 3.! .'.7 2.5 2.7 2.8 2.9 Filter my ̂

n-1 5.: v 2 3.3 2.7 2.3 2.6 3.2 : 1.B 2.6 2.7 2.8 n-1 rrACTT Us — A \ i EAST v0=2 5.8 ' 3 V 2- 5 3- 5 2- 2 M \ 3- 2 3' 5 l 6 ^ "-- l 2 - 9 2- 7 n^2

0=3 5.9 4.3 5.5 \. 2.9 ——— ̂ 3.3 \1.4 1.7 3.7 J. 7 1.9.3 2' 5 3^ 0 = 3 /X \ V. _ \ .' — x.

0=4 5.2 5 4* 5.8' -13 3.1 1.5 1.9 3.8 4.5 2.4 2.6 n-4

Line 600 W


4 —— On r®-]Filter i l i

*

^\ x /'' 0 = 25.0 M

* t * * *' - ~\ plot point , j* ***\ \; J -0 \1 . - - - ' ,,,1 \

l - -'.' 1 \-.^ \ \ ^ ;i"' " ..--w^n"^

S?^^Y^;^^O^INTERPRETATION


D Well defined increase in polarization withojt marked resistivity decrease.

D Poorly defined polarization increase with no resistivity signature .


Scale 1:250025 0 25 50 75 100 125 150

(metres)

^ '- - ; .




DAN PATRIE EXPLORATION LTD.Geoson software for the Earth Sciences

Sra

oM

ra oo

FM RES XM1 9 ( 9K54 9fl

0.60. 4827. 10. . . . . X^"**"*-^.— -*** \ . . '. . .

n (i | n i i , , i i , i . i i i i , i i T — ; -~ . i.,,

Mptnl Fnr-tor 2^5 1+50 S 1+00 S 0+50 S 0+00 0+50 N 1+00 Nniter 1-1 0.99 0.60 0.36 0.22 0.17 0.12 0.10 0.050 0.060 0.090 0.090 O.D9C

0=1

0=2 0.30 1.9 0.50 0.12 0.11 0.050 0.060 0.15 0.060 0.070 0.090 0.14

0=3 1 1.7 0.59 0.15 0.15 0.10 0.12 0.030 0.030 0.090 0.080 0.12

0-4 0.96 1.2 0.36 0.28 0.17 0.33 0.030 0.020 0.060 0060 0.060 0.14

0=5 0.61 0.49 0.69 0.29 0.43 0.060 0.020 0.050 0.040 0070 0.050 0.10

Ro^tivtty 2+00 S 1+50 S 1+00 S 0+50 S 0+00 0+50 N 1+00 NOhm-m Filter 'OT "52 30S *2" 49K 5951 ?256 "B 8776 6996 3735 3789 3746

0-1

0=2 S12 1226 1623 s 6289 9033 — 8224 5155 v 2456 -^ 5697 ^ 5615 2607 — 1927

0=3 2219 \ 1143 2156 \ 6072 ^ ~38oT~- 4793 3477 X^12K 12K ) ) 2801 4516 2156 ^- — ̂ 7 \ ~ — ' ^-, s —— ̂ //f/' "\ i ll ^

0=4 1959 1838 3556 y 2484 ! 3791 ' 1 931 //'5K -^- 20K 1 1 4623 4695 4630 2989

0=5 24S5 3187 14SO 2686 1551 '- 7892 '23K ' - 6255 6414 4194 *5765 -~ 3768

fhorqpnhility W® s 1 t50 S 1+003 f 0+50S 0+00 i 0+50 N | 1+OONmV A, pi|ter 18 17 13 11 7.8 5.4 4.6 4.1 3.6 3.1 Z.8 3 3.2

0-1

0=2 7.6 ij/j 23 i\vA^!!!^/- 7 9 y i 3 - !--^^^ 3- 6 3- 5 3- 7 2- 3 2- 80=3 23 S 20-^^7^^^9.4/5.8 4.9^^~^4^ __ 3^.9 __ ̂3.9 2.5 2.9 2.6

0=4 I9 7, 21 y) 13 l 6.9 6.4 6.3 4.3 4.3 2.6 2.9 2.9 4.1

0=5 20 -^* 16 ' ' 10 ^ 7.7 6.7 6.1 4.8 ' 3 2.7 2.9 3.2 3.7

XM RES FM .20 .9654 ..1.2

1

1 .10 L4827 .0.60

.0 Lo Lo

Metal FactorFilter

n-1 11=2

n-4 11=5

™er Ohm-m

n-1H"2

n=3

0=4

n=5

Filter mvyv

H EAST V^=3

n-4

n=5

Line 1000 W


- — dH r®-,niter i 1 1

A* ** x\ / ' a - 25 - owt t t t V

plot point

i " l i

Logarithmic l .c * \ 5 '7 ? 10 -1Contours !' ' \ J:',?' ^ ' ' ' '

* Strong Hwi'uUljl! in jjuiuiization accompanied by marked decrease in resistivity.

O Well defined increase in polarization without marked resistivity decrease .


V Low resistivity feature.

Scale 1:250025 0 25 50 75 100 125 150

(metres)




DAN PATRIE EXPLORATION LTD.Geosoft Software for the Earth Sciences

5"

o o m

H

*

1

enHin00H

P)

H0 O CM

g COofc

FM RES XM . XM RES FM 1.R, 1?K 7.1 7.1 17K ,1 fi| i i i i i i i i . i i i i i . . . . i i i j

i v^v, /""x ?0.78. 606cJ 12. \/ . ^*V*.,^ - V . . . \^ . . . .12 .6060 1-0.78

n n 1 n , , , , , i i i i , i , ,-T — i — i --i — I — I"" — ; n In j n

Mptnl Fnr-tor , 0*50 N , 1*00 N , 1*50 N ^ 2*00 N , , 2*50 N , 3*00 N Mptnl FnrtnrFilter 0.29 0.92 1.4 0.91 0.69 0.3E 0.11 0.060 0.050 0.070 0.070 0.070 Filter

0-1 0.040 0.71 1.8 0.31 0.36 0.40 0.080 0.040 0.030 C. 060 0.090 n-1

0=2 0.20 1.6 1.2 0.74 0.34 0.12 0.040 0.030 0.050 0.060 0.070 0=2

0=3 0.81 1.3 1.9 0.74 0.19 0.070 0.040 0.08) 0.080 0.070 0.060 0=3

\ 0=4 0.74 1.8 1.3 0.43 0.12 0.060 0.080 0.11 0.090 0.060 0.050 n-4

Rp-sktivity 0*50 N 1*00 N 1*50 N 2*00 N 2*50 N 3*00 N Rpsktivi+y

Ohm-m ™er 1 K KS 1 629 1 988 2427 4ra ™ 9"9 "" ** 4745 "B ™er Ohm-m

n-1 18K i j 1 786 1432 2876 2333 JIM SB -UK 12Ky 5517.^4130 n-1

0=2 *293 l 1421 \ 1 788 ^690^ 2564 6660 /12K m/ 7570 5947 ) 4430 0=2i \ ~~^ ^- — x \ \iif /V x0=3 2797 X 1575 I1J2 1598 4266 j 1IK I3K f 6300 5562 ^ 4838 5180 0=3

0-4 2690 ' 1014 1243 2658 6754 * 12K /6042 4591 4023 4893 4654 n-4

rhnrgpnhiiity , 0*50 N i 1*flO N ( 1 *50 N t 2*00 N , 2*50 N r 3*00 N rhnrrjPnhilitv

mVyv Filter 13 17 21 15 12 10 6.6 5.2 4.4 3.S 3.5 3 Filter mvyv

0=1 7.5 , 1 3 i, j 23 \v\-8.8 8.5 v^^ 12 y i 4.7 4.3 *.1 3.4 3.4 o-1 CAOT U//////l \^^^^ — l \ x" EAST V0=2 \ ^ 'Y/ n ^ —— 22;Vs;U\ 8.6 8.1 X5.3 4 3.4 3.8 3 0=2

'/^^ \X\\\\ \ \ X ^"-"~~"\ 0=3 23 20^ 2lYvi2\ 8 8.1 \ 4.8 X4 4.6 1 3.3 2.9 0=3

0=4 20 18 * 16 ^ 11 - l.t*^ 7.4^ 4.9 4.8 -3.5 3.2 2.4 o-4

Line 1200 W


' —— ®— i r~*^~~\Filter 1 1 1

*

\v/' -' ".O M

plot point

Logarithmic . i 5 2 3 5 7 S 10 Contours ]' '• bl l " *' 5 ' 7' 5 ' 1 U '"

INTERPRETATION* Strong increase in polarization


Q Well defined increase in polarization without marked resistivity decrease.

O Poorly defined polarization increase with no resistivity signature.


Scale 1:250025 0 25 50 75 100 125 150

(metres)




DAN PATRIE EXPLORATION LW.ft Geosoft Software for the Earth Sciences

\310

SATTERLY

1851

2N08SW20

FM RES XM XM RES FM 0 ?n 7594 4 , i i i i ^ ' 7WU ' " 7fl

0.099. 3797-| 2. '/. ' \ / V S N . ' ."- .2 |-3797 .0.099 1 ' " 7 \. 7 **j "-~-^/ ' -——— - i i

n! nl n iiiiiiiiiiiiiiiiiiiiiiii o lo i o

Mptnl Fnrtnr , 1+OON , , 1*50N p , 2+OON | 2+50 N , 3*03 N | 3*50 N ] Mfital FnrtnrFilter O-" 0-070 0-060 0-070 0.050 0.14 0.18 0.11 0.080 0.070 0.070 0.070 0.080 niter

0=1 0.030 0.0*0 0.15 0.10 0.29 0.26 0.03C 0.030 0.070 0.10 0.090 0.10 o-l

,^-v 0=3 0.090 0.11 0.060 0.030 0.030 0.030 0.17 0.20 0.040 0.050 0.050 0.070 0=3

•*- ^\ \ n-4 0.11 0.090 0.15 0.040 0.020 0.030 0.030 0.15 0.24 0.040 0.070 0.050 0=4

^3 \

i^' .-festivity , 1+OON p 1+50 N ( 2*03 N i 2*50 N , 3*03 N f 3*50 N , | Resistivity^^"""""^ Ohm-m ' Filter 3W 8 ' 41 5386 63S3 6904 4867 2857 6395 6624 5732 4924 4673 4028 niter Ohm-m '

0=1 10K 6182 2127 — 2250-967 1056 \x 12K 8330 4360 2661^ 3311 2761 0-1

0=2 3SK ^7177 4970 ^~6402 ' 5209^ 1374 1216 xV*' 6281 5 la9 ^3772 4536 0=2

0=3 48M 3237 5148 i 9je9 ' — IIIO*. 7718 \ 1662 — 1491 N 807/) 6459 6447 4590 0=3

n-4 2504 4833 \ 2318 ' 8732 I3K 12K ' 6733 ^- 1738 1398 - 7350 7286 7327 0=4

rhnrrjpnhili+y , ^ ^, , ^^ , 2f N , *? N , , , W" N , 3*,50N i ChnrgenhilitymV^v Filter 3.' 3.4 2.9 3.1 2.7 2.8 2.8 3 3.2 3.1 3 3.2 3 niter mV/V

0=1 3.4 2.3 3.2 2.3 2.8 2.7 3 2.9 2.9 2.6 2.9 2.7 0=1 FA^T V

0=2 i. 5 2.7 2.8 3.2 2.3 2.8 3 3.2 3 2.8 2.8 3.3 0=2

0=3 4.4 V 3.4 3.1 2.9 3.2 2.5 2.9 3 3 2.9 3 3.1 0=3

0-4 2.8 ^ 4.3 v 3.4 3.1 2.8 3.2 2.1 3.2 3.3 3 /^sT~~~~^ 3 .6 0=4

Line 1400 W


- — CD-i r®~]Filter 1 1 1

\ s\ / ' " -25.0U

S

* * * * *

plot point

Logarithmic^ i 5 9 3 5 7 5 10 Contours ' ' ' ' ' ' " '

INTERPRETATION

" Strong increase in polarization accompanied by marked decrease in resistivity.




Scale 1:250025 0 25 50 75 100 125 150

(metres)




DAN PATRIE EXPLORATION LTD.Geosoft Software for the Earth Sciences

o M m

in CD

Ho

ODOK

m RES m1.2- 2J08. 13-

.584 1154.] 6.sJ

J oJ

RES FM r13 .2308 -1 .2

L6. 5 LI154

Lo L,

Metal FactorFilter 080 0.8C J.48

1 = 1 0.46 0.24

I.I 1 0.36 O.B4 O 70 0.49 a.47 5.*5 0.52 O.J1 0.17 0.18

n-2 1.4*44^^45^.0100^1.4

1=3,, "' * \-?*4 H-n O.S2 2.1\

1=4 ^f 0 69 C 32 0.81 \

0.4B 0.19 0.33 O.OBQ -0.040 -K). 350 3. 15 O 37 0.41 0.72 0.57 0.080 O.J8 Q. OK 2. M 0.37 Q. tt 0.47 0.3* 0.40 0.93

1 l. i 0,23 D.070 0.10 C OSO O.H 0.31 0.91 1.4 0.51 -0.12 0.15 0.14 C. 11 0.14 0.21 0.63 C.8 0.15 0.18

3.* 1.5 1.2 1.4 O.M 0-C70 0.15 0.33 0.30 0.58 1.8 1.7 2.5 O.OX O.W 0.07C 0.060 0.18 0.18 0.57 O.Z4 0.11

0.79 1 17 1.2 1.5 3-13 0.12 0,36 0.54 O.S2 0.88 2.1 1 l 0.76 0.050 0.04C 0.070 O.CfiO 0-11 0.18 0.*7 0

n-2

rt*3

0.40 0.44 1 .2 0 .17 1.J 0.94 1,5 O.J3 3.36 0.42 0.39 0.31 0.75 1.00 1.2 0, O.S3 0.52 0.050 0.060 0.060 0.13 O.tS 0,34

1 2 0.72 0.93 0.86 0.030 0.040 0.070 0.0(0 0.0)0 0.11

Resistivity

0.58 2.3 067 0.81 3.31 2.5 0.65 083

1713 1535 1275 I 1483 'M IS3 '918 1977 2083 2010 1912

—— 187—- 346

1220 12S2 IMS ISM I6S6 MO

526 B13 '107 _JJ48 1052 .1108 1*42^ 1J24 ^ 2I4S --JSOS^ 1170__1043

1971 -^ 2Z32 22*4 2S9' 1722- -

fM1 V -7S3 J226 — 2895 ^ 2313^ 1441 ~ 1067^^905 846 920/ 1219 1209 2108 26'6 2898 1339 ^ 1746 1

1338 841 1035 1235 97? 1524 -^iTiS JS '"J?" - lUI1"^?? '4'2 3 I 019 1242 ~ il 9S7 4S47 335! 3375 1730 ^

1154 — 1380 — '577 1001642 -~ 1151 1069 I48B 1379 1 33B . 156*

Chargeability mv/v

n-6

4.9 1 7 "5SV{VC^T),"|4 14^—— l? —^. Ji^X; 4 .4 4 .4^5.2 9.2^ ^1!^ ~ 1 3 "fPl^j))'. "^__J'' : '-* Z' 1 L S 2 ' 5 !' ! 2' !

!.i 3.: j s.s^7~Smj~t.z~k a J i * 19 H NT":' 3.7^' 5 s 74 'ra 13 S ' zi^'-i; •~rrj\- i ;B^^!!-s 1.7 2 :.i 2.9 2.54.8^ 7 7.2 "^-u ) SS^/ 19 y^ij"\ M ' ; -^fr.;- 5 ' . "\ s ? ;"'x '.I ~^ 15 16^:!^. n ~-^,8.7 ' ̂ '^^ 2-' 2.8 2.4 !.S 2.8 2.8

i? 's-j?^; rf t! ~^~ti~^ ys——2.1 ^ ' '9 it -—'4 u 12 ' \ 2141 sis —— 7.S " 29^ 2 3 3.1 2.7

1=1 1-2 1=3 1=4 1=5

Metal Factor

Resistivity Ohm-m

.2 t 7 3.8 3 2.7 2.2 2.3 2.4 2.6

S 3.4 __46 6.5 (J ^ \J —— 1-6 IB -0.47

4__ 1.5 2.3 :.1 2.5 15.7 9.8:—— l' 2 ——24 : i 2 .3 1.2 1.5 2 22 2.1 1.7

Line 1600 S

Dipole-Dipole Array

Filter

* * *

* * * *

a = 50.0 M

plot point

Logarithmic, Contours 75 , 0

INTERPRETATION

Strong i ncrease in polarization accompanied by marked d ecrease in resistivity.

Well defined increase in polarization without marked resistivity decrease.

Poorly defined polarization increase with no resistivity s ignature.

Low "eststivity feature.

Scale 1:50C350 O 50 100 150 200 250 300

(metres)

EAST WEST/CANADIAN GOLDEN DRAGON JINDUCED POLARIZATION SURVEY


Date: 98/05/21 Interpretation: O.FATRIE

DAN PATRIE EXPLORATION LTD.son Software for the Earth Sciences

Om m

le:oi FactorFilter

7-5x 2.5 l.E O K (J. K C.55 3.75 05* 0.25 G.J] ij.ii 0.3^ 0.33 0.36 C-."8 O Z" IK

2 2.5 D.9S c.i- a : i c .3e D 31 o'S a.16 o IB o 15 o it j 19 c.:o o.is 0.5: o.K5 B G.84 2.1 2.2 077 0.57 0.21 0.23 O.J2 0.17 0.17 OH S. l* 0.15 C.17 ti.T 0 P C.37 X

1.3 i.! I.I 17 O.B 0.6C C.13 0.21 0,23 O.i' 0:6 01* O!' 3.M 0.25 O M O.K D.e:

0.7; i'. M

M C.56 O 35 024 0.;: 0.43 3 i; O 91

O 73 0.31 C-.39 B.|; o.!' C 31 C.*5

D 55 3.69 O 27 o,H o.i; D.Z? -j 14

O 4B 0.53 0.2t C.B O.fJ Q Jt

• 1 0,33

IW , 306 SK 126 (SG- — '17

19! 181 JSI 371 SI' t B53 831 1193 , 1476 1054 1374 1S52 2463 2670

low i 1 325 1677 — IK; — 144; IK1755

3033. -\ 2670 / 1525 1955 M15 IJ3: 2746 IMS 1775

1736 I56S 253J 28'0

'•WOOS 1HQOS

26 -.2 053

n-Z 4.3 y 13 i f,.} ---4,4 TTx E 5 X, i,S 1.5 3.2 1 .1 1 4 1.2 l.S 2.1

s' S 3 "12 /2.S—-^S.4 —^','———\

6.3 r '4 ) i.1 5.9 \ 13

Gs:s^ f: 2~--~iHare for tne tort/7 Sciences

Line 1700 W

ERPRETATION

.*-.;~,!yWel : defined ncrease in Do:anrciion " esistivity decrease.

2ny defied polarization inc'eose



DAN PATRIE EXPLORATION LW.

FM RES XM 14. 29K^ 60

Resistivity Ohm-m

11+SJS 10+50 S 10+00 S a-sos 7+00 S 4+505 2+50 S

filler 0.080 0.10 O ID O.I* 0.18 0.18 0.15 0.17 0.15 0,1* D.10 0.070 0.030 0.23 0,36 D.8J- 1.1 0.54 0.37 O.JS D.24 0.27 0.33 O.K O.SS

ns l D.17 0.20 0.29 0.36 0.31 0.24 0.29 D.IB 0.1! 0.050 0.050 0.050 O.DBS 0.2B I.i 3.2 013 0.14 0.18 0.25 0.23 019 O.J1 O" 1.5

1.2 1.1 0.84 O,K 0.37 o.S O.! 1 0.2' 0.12 0.070 0.070 0.050 O.i* O.It C 6i l .t 4.6 ,J ..5

3 O.J5 0.47 C.45 0.27 D.JO O.X 04* 1.080 0040 O.OK DM0 0.19 0.21 O.IS 0.3B , 5.8 x 0.99 1.5

0.060 0.10 0.11 0.15 Q.2G 0.16 0.1! O.li 014 0.14 0.040 0.030 0.040 041 0.4S e. 47 1.5 0.1J 0.20 0.16 0.27 0.21 C B 0.52 it 2.: 2.1 0.2fl Q. S3 0.50 Q. IE OSO C..07C 0.060 O.C30 0.!6 01? O 3t 35 V 5.B 2.3 4.5.

0.0*: 0.0*0 O 37Q 0.080 0.10 O 15 0.15 0.10 0.14 0.16 0.1E O 030 O 030 0.21 O.BO Q.26 0.26 1.5 0.20 0,2; 0.23 0.25 O 29 O 45 f.B 1.7 1.6 0.53 0.84 0.38 C.I? 0.13 t 15 O IS 0.03C 0.060 0.050 0.040 0.21 C.J7 2.: 3.3 4.6 ,-

0.31 a.040 0.030 COW 0.060 0.080 0.12 OJO 0.11 0.17 0.19 0.1* 0.040 0.13 0.26 0.55 0.17 0.19 1.5 0.24 0.27 0.22 0.32 0.54 1.1 19 t.! 1.4 2.9 0.60 0.73 O 2S QIC ; 1C D.1C 017 O.-CK 0.060 0.066 0.050 0.56 l .S ..2 3"~Y 2-8 '6.1- ' 1! 12 t:

I2+C05

niter

1U50S 11-KB S ..10+50 S 10*00 S 9*50 S______9+ttl S ; 3^505 SMBS______7+50 S248! 2645 2407 2322 2465 2512 3065 4038 UK 20K 20K 12K 5833 5424 4517 7KJ 7912 9121

1203 1209 908 ^__637\ s.—2486 -^ 1469 y

(153 92*32154 - 44S2 x - 20K O7K ___ 15K ^ 7238 - 45fl7 17K —— b^ ^ u.jj .L-O — - —— ~-•—~ -—- ^ _- y \^\\\ ^.^^N\\i ^ ~-^Z^NI\\\ i \ (}20J4 ^[343 ^ \m^, 2IK 2401 ( 3632 464^^22^ ^34*^-^211! ]J M12 ^ ( 4372 — 4836^- IBIS s\S9H 899! IJK l 7800 V^]^

7912 — 717'l .'STJO ' IBOt 1639 ~~~161B 1191.,, . i "i ^LCSN \\x "" \

7737 L 2066 B US __ 9061 X 1932 \ 7723 9*77 —^-^^ l ^ ~~-——-^ \-\\\ N S l i l X \^ l \ V {

5=4 2M5 3033 3851 3166 5368 4950 3237 M39 4423 2913 3183 50*2 s 3* -^ 1 4* l 7*3! 3334 \ l 12K T2f *

1192 2126 !396 3140 57P 670; EBT1 6C2: 7333 13* 17( 2* IB* ...w

5778 31B; , ,94*. 480 xN. *!ra — ZM4 3at ^^ M'- ^

68'2 f 3210' IB'7 \ mC 384! l 1945 JJ22 ( 7*85 ^ S3"VJ \ \ 7

2016 \ 4795

3190 ; 8166 ^ 1!W y 2S *•: J3V*c ^ ' XT x l w orw ;'4- \\\^-V s , : j i21TB I6M , 1093 1075

7JS - *5c Ml 347

S**9 7434 45V 2HE IRK

7044 ~ E782 912f * 5291 ~~ 3502 24&S'' 1737 '2353 2118

SZ7 5995 . \ 211! 29K 39K , , , , .^. , .. . .... .~^ \\\\ \ \\VV, ^ /{ ~~~^\

BCil 6774 " 23. 2fl* 33" ^ 414J — JQ2J j(2! IB

Chcrgeabii'V, mV/V

12+00 S 11-KOS 10+50S 10+00 S 9*50S 9*COS 8*505 7KOS 5+5DS 5+OOS i+OOS 1*005 0+50:

niter t2 13 II 29 37 M M 54 4? 375.7 B 9.B 11 12 17 21 K l ? 18 20 K 23 252.1 2.7 Z.9 3 J.2 J.S

2.4 2.6 2.3 2.3 2.4 2.9 3. B 5.* 9.* 9.1

2.6 2.6 2.7 3.5 5.1 S.S 9.2 r 10

S.! 6.5 9.9 li ^-* 16 17 21 23 v ZS3.4 3.3 3.8 J.7

IE 17 2- 571.2 1.9 3.3 3.7 3.9 3.7 5.1 ——— 5.1 5 9 7.2


0in m

!M

iS ra

o*Hin eaH

c*

Ho0 N

m ofcMm

FM RES XM 0.57., 2485,. 7.7

0.29. 1242. 3.9.

0- 0. 0.

Metal Factorniter

0=1

0=2 0 0=3

0=4

0=5

11=6 i

Resistivity ^ r-^-v —— v^ ' ——— ' —————— ' ——— ' ——

N x

^-— -*~"--— ——--c""

11*005 10*005 9*005 8*OOS

0.37 0.26 0.27 0.23 0.23 0.22 0.27 0.3

0.25 0.23 0.42 0.42 0.46 0.38 0.39 0.30

79 0.15 0.23 0.28 0.23 0.26 0.20 0.25

0.56 0.25 0.16 0.17 0.19 0.21 0.16 0.22 , ••-"^\

0.79 f*\® \ 0.12 0.14 0.15 0.16 0.060

t | "i ;*0\Jf 0.\ 0.10 0.16 0.14 0.35 0.41

", " \ "' "' "' "

iv- J \kdjSSf^ lOjjWT 9*00 S 8*003

Q. J HWr -'^ l"P,r\:UJ6-''*'"8 '219 1177 1089 945 807

r\~\^'*ySI m 520 ^ 394 ^263 —— 2B TO (34

0=3

0=4

0=5

0=6

Chcrgeaoi;i:vmV/V Filter

0=1

0 = 2 4

0=3

0=4

0=5

0=6

740 f 1157 1153 1128 11*T~~967 \865 578

892V 1206 1583 ~ 161?" iw 991 766 — -.

906 1549 215 21i3\ 1654 1144 VJ !71

I1Z5 ' 1971 2787 2118 1812 x 1242 '

11+005 10*00 S | 9*005 8*005

3 2.6 2.7 2.3 2.2 2 2.2 2.4

1.5 15 2.2 1.6 1.2 1.1 1.6 1.3

7 1.4 2.3 2.1 1.7 1.6 1.4 1.3

4.1 2.9 1.8 2 2.2 2 1.1 1.3

7\ 2 2 2.3 2.5 1.6 0.44

4.7 1.7 2.2 3.4 2.3 4 3.6

3.9 3.4 3.1 3 2.4 3.6

XM RES FM

x-~^-x^*rrr:^\^\ ^'" '•-/--^--^^---- ———— ' ^""7 ——— '"~— — -3.9 1-1242 r0.29

'o^ ~"--- lr i

7+pos . { .6*005 5*00 s 4-00 s 3*005 2+00 s inns Metal Factor0.28 0.28 0.29 0.29 0.30 0.49 0.47 0.52 0.44 0.52 0.34 0.26 0.21 0.18 niter

0.19 0.13 0.24 0.27 0.22 0.79 a. 52 0.71 0.26 0.86 0.12 0.15 0.18 0.15 0=1

0.23 0.12 0.13 0.21 0.17 0.28 0.63 0.42 0.77 0.61 0.58 0.27 0.12 0.20 0=2

0.27 0.15 0.16 0.22 0.30 0.52 0.71 0.38 0.53 0.48 0.61 0.39 0.11 0-3

0.52 0.52 O.'l 0.19 0.28 0.44 0.40 0.53 0.26 0.69 0.37 0.19 0.050 0-4

0.90 0.86 0.12 0.28 0.37 0.53 0.36 0.35 0.34 0.33 0.19 0.27 0=5

0.34 0.38 0.41 0.24 0.33 0.48 0.44 0.39 0.39 0.37 0.44 0.54 0=6

7*00 s 6*oos 5*oos 4-00 s 3*oos 2+00 s i*oo s Resistivity1521 1893 1927 1835 1832 1512 1581 1461 1381 1336 1458 1874 2141 2259 niter Ohm-m

NV 1727 — 1661 1426 1151^.1362 xKI ^ 9J* —^515 542 563 782 1BI^1544 __ , 195* 0=1

718 l J 2951 Wl\^TX^, Z050 I*34 "2* 1484^926 809 785 ( 1 794 2815 2793 0=2

761 NX 2999 2484 2155 1333 1514 1207 \ 1684 \1 121 V-JJ2 ^-— 953^ 1552 j 2996 0=3

660 793 \\ 3096^ 2740 1859 V M27 1790^ 1513 1878^ 1233 1331 l 2515 2351 0=4

^697 ^V, 3582 ) 2308 W 1866 1650 ( 2422 2114 2401 'x 1672 I84e ~ 1650 0=5

836 ^ 673 ^975^ 2603 2107 1683 1770 2256 21t4 2861 2066 1600 0=6

7+OOS t 6+pOS t 5*005 , 4-00 S , 3+ODS : 2+005 : 1 *(10S Hhnrgpnhility3.3 4 4.5 4.8 5.4 6.6 7 6.8 5.9 5.8 4.8 4.4 4.2 3.8 niter mV/V

-V2 3 3.5 3.2 3 4.9 *' 7 -^ j:7 ''* 4 i8 0' 97 2 2- 8 3 ^ ^

1.7 3.5 3.3 3.6 3.4 4 / 7 .1 6.3 7.2^^4.9 4.6 __ 4.9 ^ 3.3 Sil 0=2

2 4.5 4 4.8 4 f 7 .9 1.5 6.4 6 ^ 4. S t 5 .8 6.O 3.4 0=3

3. t 42 __ 3.5 5.1 5.1 — '^6.3 7.1 E. 8 5 8.5 4.9 ——— 4.8 1.1 0=4

C (-2 ' -5 j 4.1 l 6.4 7 8.8 6.8 7.4 8.2 5.5 ^3.1 4.4 0=5

2.9 2.6 4 ^6.3 6.9 8.3 7.8 8.1 8.5 9.8 9.1 8.6 0=6

Line 20OO W


' ——— (Eh r-®-! niter 1 i 1

*

* * \ '* * * ^x / ' a " '

* * * * . ^8 .plot point

Logarithmic 1152357^10Contours

INTERPRETATIONB Strong increase in polarization



O Poorly defined polarization increase with no resistivity signature.


Scale 1:5OOO50 0 50 100 ISO 200 250 300

(metres)

EAST WEST/CANADIAN GOLDEN DRAGOhINDUCED POLARIZATION SURVEY


Date: 98/05/21 Interpretation: D . PATRIE

DAN PATRIE EXPLORATION LW.Geosoft Software ror tne tarth Sciences

oIDm Ohrri-m

r3

LO

n-2

0=3

0=4

0.77 0.91 0.27 077 J.WO 0.26 1 .72 0 .26 C.32 0.25 C.26 0.35 517 ; le 04? 1.1 1 0.(3 Q 75 022 C 30 5.3* 5.4! [76 -1=1

3.57 1.1 G.K 0.2E 0.67 0.3E C 25 C 21 C.M 0.18 010 0.21 521 314 5.S 0.63 O.ffi C.76 0.3t 9." 0.1] C.23 D.3* C *9 -1=2

0.74 Q.76 O 50 O 21 0.10 D 15 3-11 Ci K O OBP fl.EBO li OSO D.10 3 14 C.23 C.45 O 36 0.33 fl.JE 0.26 O 19 O M 0.13 0.22 r^3

1.4 1.2 O.B9 0.6F C.I 1 Q.19 C.21 C 13 O.'l B. OH- 0.14 OH D;, 3.54 5.55 O.T; 5.4; c.;- D. 45 3.24 5.36 C.'o 0.31 n^i

D. 10 r-,^5

7SC ^ 913 ~- 1 276 — 1636

ME ^ 172- — 1633 — 1S52 135C — 13S3 — 1631 -" 22J4 — Jfll*

1M7 -960 4072 5W4 7198 722^ 4047 (JS7 4422 f (258 TfSIISO! 1MS 2072 ,- 3710 396?

Cncrgeaoi'itymV/V Fi ' ter

11=3

0=4

2+00 S

6.

} 3.2 1.0C 2.E 0.3"^ 0.97 0.75 i.3 2 2.5 2.E 3.2

2.3 .'6.7 \4 1.9 i 7/) 2.7 l.o 1,5 l.B 2.3 1.1 4'

74 5 8.1 "TT———5.2 2.4 j.: 1 .1 1 .S 1.9 0.85 3.S 4,*

5.S 7.3 7 3 a .-) j 1 .9 3.3 3.2 1.7 15 0.81 3.1 4.i /'

7.4 6.9 7.5 a.9--^^Tr ,3.' 3 3.i 2.7 2.2 1.5 31 3.6^^,53

-''.2'^ 5.6 6.5 ' 17 ' 6.2 5.1 2.6 *-1 4.3 5 I.E 4.! 6.6

/i] X. a

i 3-^ 1 1 11 13 1 3 J ? l 4.t 1 .1. / i-2

'' II r II' 13 11 '-, 7.1 ^"~ M ~~5.5

II lil 12 12 i! 14 11 7.3 9.J 0=6

Line 2 200 W

INTERPRETATION

accoriponec oy Tat b. resistivity

50 O



Date: 95/05/2' Interpretation: D.PATRiE

DAN PATRIE EXPLORATION LTD.

o r*- m

H

SD]

inCO

o o(N

FM 3ES XM ' XM RES FM0.92. 34K n 31 —— , —— , —— , —— , —— , —— , —— , —— , —— , —— , —— , —— , —— , —— , —— , ———— , —— , —— , —— , —— , —— . —— , —— , —— , —— , —— , —— , —— , —— , ———— , —— , —— , —— , —— , —— , —— , —— , —— , —— , —— , —— , —— , —— , —— , —— , ———— 31 f34K .0.92

\ ^^^j^' XN f0.46. -7KJ 16. \ / ^""-^ \ f~~~~^^^ - 16 h 17K '0 ' 46

i ^^ ^^--^^-^ ^---C" ^OXL i lni nl n i,,,i,j,iii l i, ——— i — i — i — i — i — . , , i i.. . i i i , , i : , i i ..., .1,111 n in in

Uatnl F^r^A , 0*50 N | ^ MEN , MO N ] 2^00 N , 2*50 N ( 3*00 N i MO N , 4KB N | "50 N , 5*00 N i 5t50N f 6tXN t M atn | Fnr^r";; \ n iter 0.8* 0.55 0.29 0.13 0.090 0.13 0.2Z 0.35 0.36 0.33 O.Z5 0.47 0.50 0.38 0.28 0.18 0.13 0.11 0.090 0.090 0.080 0.050 0.050 0.23 0.34 Filter

\ ' \ 0=1 1 0.60 028 0.060 0060 0.040 0030 0.19 0.30 0.38 0 0.3B 0.39 0.22 0.21 0.12 0.070 0.10 0.10 O.OBO 0.090 0.030 0.030 0.22 0=1

t - -0 = 2 0.8B 0.30 0.18 0.050 0.050 0.020 0.25 O.Z7 O.JO 0.01DO 0.20 0.64 0.37 O.Z5 0.16 0.15 0.10 O.OBO 0.080 0.10 0.040 0.0*0 0.040 0.71 n~2

0=3 0.50 0,36 0.070 0.050 0030 0.35 3.12 0.27 0.25 0.39 0.53 O.S8 0.44 O.H 0.20 0.15 0.090 0.010 0.090 0.10 0.050 0.050 0.050 0.56 0=3

^ - ' 0 =44 0.39 0.23 0.040 0.030 0.52 0.61 0.64 0.72 0.22 0.43 0.64 D.83 0.40 9.Z6 O.Zt 0.14 0.090 0.090 0.11 0.10 0.060 0.050 0.040 0.29 0=4

Ohrn-rn Filter 3769 6037 IX Z* 30K 31K Z4K 1671 rao 106! 1362 1565 2009 3439 5620 7999 UK 1ZK 1* ISK IX 1X I2K 6903 5961 Filter Ohm-m

0=1 1889 i 3830 ^ 7058 \ sZTK ZSK 29K ^x^f 204* ' ^ —— 339^^289-3=^744 .2537 5244 7381 M38 13K IK IIK IX IK !2K I2K v 3745 0=1

0=2 3199 , 6109 ' I 3K J 28K 30K - 49K 11 2255 — '.OS ™ —— 5 71 'f \m ' 674 2113 — 37S6 V 9738 9162 -V IIK ISK - —— ' 1SX IX IIK IIK IIK A\789 n-2

0=3 65W^^- 9558 //26K^^^Z6K /57K /2210 '273 '060 .^SaT^ J230 ) 2307 i 1372 1478 \ 4565^ 8419 8595 \ 13K l 1 W (l4K /^"isfN 12K 12K 11Ky\ 1067 0=3

0=4 1724 IK ' W i9K - 1993 1281 963 920 -^ 2467 3099 '588 1098 1693^ 3879 7395 UK '17K I6K I7K 1* I2K I2K 1X^~230S 0=4

y i . Fj[ter 25 28 25 20 16 12 9.2 5.4 4.1 3.6 4.6 7.1 9.6 10 IZ 13 1Z 13 13 13 11 7.3 5,5 6.4 5? Filter mV/V

n-1 20 23 20 17 __ .16, 11 -9.3 (. 3.9 2.6 1.3 00100 2.8 9.8 ^13 15 t! -9.3,, 11 11 11 9.) s 3 .5 3.3 i 8.4 0=1

0=3 32 J4 \\ " \ 'J (j? l ™ 5 -3 2.' ^-5.2. __ 4.J s '2 9 .3 6.5 10 \" \ l] " " " /" ^ s\ 5- 9 5-' 5.5 S "^1 \ \ x / ^x -S s { \ \^ V J N \

Line 2400 W

Pole-Dipole Array0 na a

—— CD-i H2HFiltPr 1 1 i

.Y.* * * * , . *" . . plot point

Logarithmic . 15935 75 10Contours ' ' ' ' ' '

INTERPRETATION



C Poorly defined polarization increase with no resistivity signature .

w Low resistivity feature.

Scale 1:250026 0 25 50 75 100 125 150

(metres)

EAST WEST/CANADIAN GOLDEN DRAGONINDUCED POLARIZATION SURVEY



DAN PATRIE EXPLORATION LTD

M

J

t Software T'or tne fzrtn Sciences

9*005 7+005 2*ras

n^ ! B.Zl 0.53 l 4 0.26 11 1.2 4.3 O.K C.35 O 67 15 O 84 C E7 0.35 04? J JJ C.31 0.2' C.11 O,If' t'.

71=1 026 ea? 1.6 1.3 0.4; 1.i t 0.5S 3.M O 61 D.'l Z f. t'J 0 25 5.Zi 2.18 C '5 O.S6CI 0.090 Q.3U

n*3 O 79 '.3 0.76 D.5J 0.41 0.74 0.79 C.E3 045 0.54 0.46 C 36 0.32 015 3 14 CM 0.06G O OSO 0.2s

0=4 C-94 5.73 0.55 0.34 C 46 0.59 0.75 064 Q.75 0.40 D.E C 2e B.I? O OK C.i: 0060 O.M3 0.2! 09'

n^S 0.50 0.46 0.39 0.15 C.3E 0.53 1.68 D 4B C.33 G.ZB 022 A . li 015 D.C7C C.C5C D.OBO O.)l 0.7'

'.l 0.5?

:.l 2 .77 CS7 0.7E &.4T Gil

11 O 53 0.55 "i.K C .3:

l 2 0-75 0.51 0.51 fi.56 C K

3.55 O 51 0.5C Q 4? C.2:

!.4S 040 O.*g D.11 O 29 O li

1140CS 7*031 yras

?' y 1233 '323 B70 vB37 y SK

15JS l ISO . v 635

12W (S22 ^ 992^^~J577

1124 12K ^ 1461

1603 law 1569 ^ 2047

^=E

Line 2400 W

plot Dctnt

INTERPRETATION



Date; 93/05/21 interpretation: D.PATR1E

DAN PXmiE EXPLORATION LTD.

0.75J 13B7,

OJ Oj C.

Metal Factor

O Oim

&KC S

0.70 l 1.3 1.1 2.E O 53 0.33 O.K ' T 5 41 B.0*3 O.Z7 (j c 0.4S 0.32 :.30 O 33 O M O 64 1.5 [i 25 '5.22 l 0.25 5.3; C.5!. O 7! J.f3 r—l

0.52 0.78 1.4 1.4 1.8 1.3 G.33 D. W 0.5: C 7i o 20 0.0100 G. 14 0.21 C 2E 3.25 0.20 0.30 O.K 0.63 1.5 0." C. IE O M OH Q ;6 Q 30 0. 4E r - 2

0.61 C.76 1.7 1.3 14 0.63 0.51 0*5 135 0.50 0.26 0030 C. M v .23 0.30 C.25 0.26 D 50 O.B9 0.6' '.* 0.42 015 0.45 Q.i: f .'l 0 30 r^

0.59 0.69 1.4 1.3 1.4 l 0.51 C.35 ! Z' G 3fl O 13 0.050 0.13 O Zi 03* c.S3 0.40 0.59 0.16 0.5E l 00 0.33 0/2 D.32 0.13 O \ i r=i

C.53 0.39 1.4 0.55 0.55 0.73 0.33 l .H 0 21 0.30 0.14 0.0'Q 0.17 3.25 a.42 d.47 O 4B 0.53 0.69 D 47 O.B* D X 0 .11 0.3C C.K r^5

D.31 0.49 1.6 11 C.79 Q.7i C.3? H 2! D.'E 026 0.1E 0.11 021 S 37 OJO 3.56 0.4f 0.50 O.K O." 0.75 032 0.12 0.29 r^o

12+CQS HWM: WES•4KDS_______1340QS ____________ ______________________ |___________ _____________________________.—..^___________^—^——-^ l ter 1 t76 1W1 s?1 336 636 9*2 11B2 1471 lElj '7J3 17W 1705 1671 1&51 1*1* 220? 2307 2152 2245 IBBi 157S 2503 tZK JM4 K4U !4.'l ffiB" 1*77 Filter

[1=4

10C5 " 116! 1S67 2036 2527 2225

1912 1 377 *70 X 503 Zi53 303? 2'10 1633 X 21J4 - '22? 1 2S2f ^ MSS 2713 —

Z097 1322 -x- 534 653 f 833 652 \ 1303 7 1 852 171! 1021 — 1917 — 1335 ^ 1SK 1755 ;ul!t 276! 3133 239C x, IB!' 246E ^- 1653 3412 . J678 ^ 21S5 J6if

1935 — !E6i X 615 l 844 501' 3104 137C 2*31 4SBo 263' 'l *12Z

2723 1951 ^ 777 823 10C2 1Z55 2097 SIB M77 3246 Z6(6 2495 236! 314! 20J5 2=13 291: 2649 2379 - 3*12

•4-WBS 12-tOOS

S.9 E.!

5.8 ~ H- 5 .9 5.2 B.4 .3.5 24 44\ ,/

^^.9.1 7.1 7,1 1Q\ !.3 ^ *.1 4.6'' t.5

12 10 i 8.2 7.6 9.6 5,: 5.6 5.6

12 /S-l 7.6 B.2 V^nJ^; B.B c.6 6.1

'O 7.3 3.B 5.4 7.5 7 E 5.5

B.6 9.6 12 -~ fl.6 7.9 5.5 6 '

v 1.7 D.I6 T 1.9 2.7 3.7

75 \ 2.2 O.WO 1.4 Z.5 3.6

7.9 \3.5 0.5C 1.7 3.2 4.g

i 4 7 7 \ 3.5 0.32 2.5 4 l

5.7 8 \3.E 1.7 3.5 5.3

W \ "X16 ^ M.S X 4.3 \ 6.6 X 3.3

leto: FaciQr

Resistivity Ohm-m i

Line 2600 W

Logarithmic Contours

INTERPRETATION




DAN PATRIE EXPLORATION LTD.

m R ES FU

2 1.

oJ

'.ci Racier 3*50 N "-KB N 7-teO N 8-OON MON WON ItKOfJ1.41 0.43 0.16 0.22 0.1; 0.070 0.060 0.060 0.080 0.090 O.M 3.090 0.090 Filter

, '.A. 0 .:C MG O.:o

i ;.z' 4.1 :: o SE MS -I.OTG 3.3531.37 j.J 1 5 2.3 '!-SJ. Q.i; G 060

'5 1.5 1.7 3.E- 05J a.11 3.i4

o : ac 0.030 OKO 311 a K 329 032 1. 1- 1 .1 c;? 0.43 0.41 ;;i o. m o.2' 0.13 3 M M4 o.w o 71 c 17 o is 0040 o.ow c.10 o.oeo 0,11 0.11 o.is o.to•j ' 3 5-30 3050 O OSO 0.23 0.32 0.57 i J i,j 3.35 Q 75 'j.TT 0.79 016 0.20 0.2E J.'5 3.15 3.75 ; 56 C.J-6 022 0.0*0 0.030 0.050 0.070 l.090 0.11 0.11 0.060

J 3 SO 0.350 3.050 0.15 O IT 3.74 O.S : 3S I.J7 ' - '.T 13 3.21 0.11] 0.2J Q.:6 O 17 O 97 j.57 Q.27 0.2t O JO O.id 0.040 0.020 0.060 0.070 S.10 0.090 O.Offl 0.10

: wo o.ti 0050 3o?3 o.i* g.a 1.1 057 3 ~i '- ;.s ; 3,3* 3 is 0.25 t .n 3 25 ' n.63 1.2? c.21 0.43 0.25 0.20 DOT 0.020 ooso LOW 0.090 o.oro g.ii--"~~o.io

o o

•i.2 S. 7 i .4- 6.5 i.4 4.,

,:/ l

i? is *" i;

5.1 45 T.C 5.3

5.1 s. 4 ;s J'S.* S, l l 6 8

7. E D. B M 6. B 62 5 3.'

Line 2600 W

Pole-D'pole Arrava na

plot point

Logarithmic , Contours

INTERPRETATION

Strong increase '~ cO'ar'zaticn accompanied by marKed decrease In resistivity.

Low resistivity feature

Scale 1:2500O C5 50 ^ 5 "DO 125 '50

EAST WEST/CANADIAN GOLDEN DRAGONINDUCED POLARIZATION SURVEY


Date: ge/Oo/.C^ Interpretation: D.^VPIE

DAN PATRIE EXPLORATION LTD

or-l

FM RES X U,-5flK

l

[

l. .39 L29K .95

Lo

RESISTIVITYQhm-m

D.OK O,ON 0,050 O.DW 0.050 0.01] 0.060 0.060

15 ozo a at H o.oioo o.oino o one a .mtK 5 .11 3 ojj o.n o.3f O.B 0.34 D.I: g.zo o.ow j.ti o.nw j.oo D.OM i ,m o rea.47 O.KU D.01CD B 0100 10131 D.OtOO D.IE 1.5 O.B 2.8 O.K 0.41 O 11 0.14 O.S J.(SO O.MO O.ON Q.fflO O.Offi 0.090 0-W5 O.OiH

0.4! O.CS a.(M (I.OIM O.OIOD O.IS I.I 0.50 I.] 7.7 ___L! O.B 0.17 311 O.U 0.0(0 O.OW 0.060 O.OJO O.OM O.OSfi O.DKJ 0.050

I.! 0.37 C. tt JKt D.CZO 0.020 O.U l.S O.SI 1.8 1.5 0.51 S IS 1.6 5.1! B.W WHO O.OW 0.050 O.I) O.OEB O.CB3 0.060 B.OSO

!M 4B !1IO 2113 IX J7( i!K MK ]* 60S 2KZ ISt JW B* 171 MN

1-tOON 1-53 N

6.1 S S-t 6 i -- 12 7

5.B f.Z 6.7 ,/ H r 2Z

6.S S.6 6.8 ,/ IS ." 22

T.7 M S li /J} a !Q -" S ' tt

K 12 II 10

V.

i.: s.? e.t

, 13-^,20 14 , S.7 B.J B 7.4 8 (J , 1.7 J.I n-1( Js^ \ j V^,-——^ l j

ZD -^ .Z* IB l 'l 12 9.7 S.5 66 S.B 4.8 J.7 s 9 .5 n^2

li --- 16 -\ 15 11 . 8.1 6.) i.2' 1.6 IB !-7 n-i\, \ ~*~^ / ~~

1 17 '9 16^ 14 9.4 85 S.8

MCTAL FACTOR

RESISTIVITY Oh m-m

CHARGABILITY

Line 2750 W

Pole-Dipole Array

Rlter

tt* * * * *

plat point

Logarithmic Contours

INTERPRETATION

* Strong increase in polarizationaccompanied by marked decrease in resistivity,

Q Well defined increase in polarization without marked resistivity decrease.


T Lour resistivity feature.

Sco!e 1:250025 O 25 50 75 100 125 150



Date: 98/05/20Interpretation: D.PATRIE

DAN PATRIE EXPLORATIONSoftware 'or (fie

y840052K08SW2001 2.18519 SATTERLY LAKE 420

FM ÊS X M

1

\

5.3. Z31QK-I 5.4.

J -

Q J oj c.

Factor 2niter

\^ ^-^ ^ -A \

WQS 19-KJOS . 15+00 S 17+00 S 16tCOS 15+00 S 14*00 S 13*005 '2+00 S 11+03 S 10+03 S 9+00 S 3KO S 7+00 S 6-00 S WO S 4tCO S MO S 2KB S 1-0)5

XM RES FM 11 .-4620K ^11

[.5.4 1-2310K .5.3

t

o Lo Lo

Metal Factor1.6 1.2 1.1 0.31 0.63 5.56 i, 56 0.63 0.72 0.65 0.45 0.31 C ;- 0.33 0.33 3.40 3. is 0.32 0.28 0,21 0.29 Q. 31 0.19 0.15 0.15 0.16 0.15 1. 13 0,11 Q. 10 0.1! g.|5 0.13 2.7 3.' 35 6 3.7 9.5 i Filter

1.3 1.3 O.M OSO 12 1.4 1.7 !.4 0.86 9.5E "i 0.91 0.37 3.95 0 E5 0.52 U.*S 0.36 0.72 080 0 2B 0.26 0.32 0.30 0.25 0.14 0.10 0.070 5.10 0.10 0.63 0.11 (MS 0 0.15 0.7 n^l

Line 2800 W

ôle-Dipo!e A -a na

Filter i i* "'x* *

* * * s , '

t r * * b' plot point

O.SO 0.71 0.63 0.K 0.44 O.B* C.35 l 0.63 020 0.25 133 035 340 G.46 0.11 O f. 0 .21 0.25 0.54 D.19 O H5 0.16 0.16 017 0.16 0.10 0.060 0.050 0.030 O.Sfl O.OSO 0.32 O 0.61

1 6 0.69 0.57 0.54- Q 51 1.33 0.46 O 68 0.70 0.57 0.2* :.*- 0.25 0.28 123 O.E3 0.40 D.19 0.20 0.22 O 25 O 26 D.12 Q.11 0.13 3.16 0.15 D.OSO 0.060 0.070 0.36 0.090 D.16 O i J 2.2

2.5 1.1 d.59 0.61 0.5S ;.** 0.23 0.33 0.52 &M 0.32 023 310 315 3.21 3.24 0.46 0.23 0.13 0.16 0.16 0.17 0/9 0.11 0.10 013 017 5.11 0.090 D 060 0.23 0.060 0.11 O 3.f 2) 0-86

4 25 1.3 D 69 0.56 O 50 0.33 0.25 a.JO 0.39 0.37 0.26 5 'E D. 10 0.13 :.1B O '9 O 19 0.23 O 17 0.15 0.12 D 15 0.15 O.OM 0.10 3.15 0.14 0.13 C.10 D. 19 O.OW 0.053 O O 47 ""L^F 1.6 6.1

1.3 1.5 '-4 Q.65 B.5C C.13 0.3* C.21 Q 22 0.33 0.33 0.2' 3.13 3 090 3.1J C. 17 Q. 13 0.17 D.20 0.15 0.11 O.ld O.'l 0.13 0.070 3.080 0.080 a.16 0.16 0.36 D.040 0.040 O 0.39 1 .i'^^Mlf**^'.3

13+00 S 7*03 1)00 S

995 ''.37 1175 1702 1 603 1 408 '243 1147 10 -14 -151 12B5 1 *B 1613 1575 1 513 1 551 1643 B5S JI45 2B4K 617V 1589* 2119K HMK 330 136 MB Filter

36 \tftfîfstivity

446 ——— W. ——— 164

77} 590 —-. 9.15

533 l '06J

1329 . 2952 6278 — E665 37E9 J393 -j 3 17 -^. 4072 MB ICWOKV

402 -540 603 -- S4

'21 ^*- 1067 1579 1928 — 20*5

rtE 1263^ 162f 2119 ?377 ^ 1972 . 5921 -7 " 'IK "^-.6857

•~- 1380 S 1 S'6 2372 2253

6401 7 113 -OOOOK ,E76JP/— 7054 IOOOOK

34*2 !W6 1580 1143 Ii3l ^ 'S5 172C UJJ I6JO -^ :i55 -^ I7i? 176! 3121 2278 2705 2222 —- l W l 25K 2433 2355 2814 2172 K45 — 456:-4^^-^ffit/ ^^^rm\/^17 — f4K __s 1 411 ' 10000! 2271^ 63 —— '68 '

3WBS 19*005 1S*005

IBS; :OEC 242' *26I 4045

16+COS

2564 29J6 31EJ — 29'2

ICWffiS WB5 7*00 S

2636 24J5 "~ 2274 "^-

6-COS

l SK 7 lODOC* 1530 9*0 ——— *4

JK10S

3.5 7.9 1.5 6.6

5.9 i.* v 3.3

E. 2 -7 5. 3"-- '.S

3. 6 7.3 '.2 6.!

9 l 9. J 7-3 G. 2 7.5

3. i tO fl. E 3.3 S. 6

x 9." S.I 9.1 E. B 95

7.3 6.6 5.9 5 i.j i.3

i 3 -^3-4 .'2 J 23 ' .i

5.7 4.8 43 j 1 l .Z

7 7.8 --^X 4- : "- 3 ;

7.9 3.6 5 - l 3 3.3

7 S 5.6 E.9 6.2 \ 4 l 3.5

i.' 3.3 3.1 3 3.2 3 24 2.? 2.J 1.5 3.1 3.B b.l 5.1 i.: 5.6

28 2.5 2 2.1 2.9 2.5 '1 li 1.9 2.5 3.3 *2 x 62 s 3.3 3.6 3.5

5.1 "liter

i.6 , l i , 1 .9 . 5.' 75' S \ '-^

32 5-5 7,Z 4.3

2.5 Z.4 2.6

M 2,2 26

O.M 3.? 2.4 2.7 2.3 2.8 1.4 1.7 2.3 33 3.2 4.2 s, E.4 \ 1.8 3 B S 6 3 5.5 s—-. \ \ X 'X N -^ A~7.2 ^ 3.6 3 2.S 3,2 3.1 2.9 1.5 t .7 2.5 i.* 2,9 47 6.3 ^4.7-^ 6.1 5.9 , \2 1 5 S .e 6.2 4 !^/ 5 7 r-r^J

*~——*' 3.7 3.i 3 3.2 3 2,6 19 2.3 3 3.6 2.7 5.3 73 6E 53 7.7 '.G-, 'I.——-54 5-3 6.2 [1=4V \ , Y \

i.E 3.4 41 3.7 3.3 l i 3 .3 26 2.J 2) 3.5 4 5 5.5 9.4 5.5 7.2 5.8

S3 S S 7 t 6 .1 63 5.2 55 7 1

Contours

INTERPRETATION

Poorly defined polarization with no resistivity '

Scale 1:500050 O___50 100 150 2

i — ' __ L (metres)

EAST WEST/CANADIAN GOLDEÎNDUCED POLARIZATION S

SATTERLY CLAIMS SATTERLY LAKE ARE

l r, t-r P Ration: D.PATRii

PATRIE EXPLORATJQ

On

!HtlK W

rt! W

inCO

oo

Min

FM RES XM 0.7U '9K-, 27^

0.36. 9343-1 13.

OJ oJ 0.

XM RES FM 27 19K .0.71

.0 LO LO

MptnlFilter 0-66 0.59 0.22 0.34 0.41 O.S3 0.33 0.22 0.17 0.10 0.14 0.12 0.17 0.13 0.17 0.11 0.12 0/4 0.17 0.20 0.23 0.11 0.090 0.070 Filter

"^ - 17 ~0 - 02C o 35 0 ^ 0-u "^ 0' 56 :' 51 Q' n Q' 070 O' t2 Q' H 0' 080 Q'Qfc0 0'MO ^'^ 0-12 c~ 11 0'03D 0* 080 Q' !l Q' 37 fl '030 0' 070 n s1.n^jj \ 0.76 1.5 0.29 0.24 -0.020 1-Z 0.*3 0.24 0.25 0.060 -0.020 -0.23 0.040 C. 090 X24 5.090 0.10 0.12 0.12 0.15 0.22 0.20 0.060 0.040 n=2

" r^3 \ 2.9 H). 13 0.020 0.20 0.76 0.26 -0.1' 041 0.14 0.16 0.11 0.51 0.18 a.23 0.12 0.14 -0.07C 0.20 0.37 0.22 Q. IB 0.19 0.040 0.12 [7=0

0=4 Sj -O.S4 0.81 0.090 0.54 0 13 O.Z3 0.67 0.370 O.OSO 0070 0.32 0.13 O.I! ).1( 0.030 0.030 0.42 0.19 0.15 0.10 0.19 0.14 O.OW 0.040 11=4

2*S)N }KX)N 5*00 N WON 6*00 N

Filter 232! 1051 937 716 B02 923 1143 1606 2B2 4281 M03 S646 8759 UK "OK B837 13K 13K !9C

3931 , 1156 -^ Tit , fSI 306 3C5 386 -- 867 ^ 1525 - 5537 ^ 7545 451) , I^ \\ <<l. //^ \\\ i i i -- '194 i:o ) 644 535 —— 495 __ . 47! .-^ 1 13) 1297 2074 V 7750 ?!44 I3W

!34 — ̂ 892 ^ 1 035 ^11! ~ __ 700X^1704 1681 — " 1656 J441 ~ 456F 6317 8042

1020 ^2510 2419 2140 3573 '~!?i3S3 - 1249 13S3

IOK ISH '411 . , 5230 : 1 2K 10K , W 1* , 8876/l s 7 \ \ \\ 1* 1 !VO 734B y "" '* '* V^J* '*

I5K 1IK 3873 1SK 14K 17K

8876 6642 , 20K . 9440~ 'Filter

n-t

"K^/ 5582 .' lil 1W /I7?\ I2K m 1 11 12K T641 18K 15K

5t07 7501 (W ~" itx S230 13K ' I 8K I5K 9292 —— 10K 1* 9SI4 S 1 3K 18K -^

F'lter !-7 7.2 6.3 1.5 2.4 2.9 44 t S 4.2 5.2 6.3 82 10 15 12 15 20 24 22 21 13 11 12

n^l

0=2

15 ~— 14 —— li nz4

Fnrtnr

Ohm-m

Chargeability mv/v

Line 2800 W

Pole-Dipole Arrayo na____ a

f^l

* *

* * * *

0=25.0 M

plot point

Logarithmic . . ,- Contours 5. 7.5. 10,.

INTERPRETATION

B Strong increase in polarizationaccompanied by marked decrease in resistivity.



V Low resistivity feature .

Scale 1:2500O 25 50 75 100 125 150

i (metres)




DAN PATRK EXPLORATION LTD.eosoft Software 'or tr-e zartn Sciences

3H EH

Ol

inCO

ra oo

CM 10

FM RES XM XM RES FM

12. 15K-I 19. \ ^"\^-7\ \. /' S*^^~~" - 19 I-' 5K - 12

l 7 \ NX .̂ \l \/ V-~~~. — - --- /^ —— -^ ^- 'n n l n . ^ — ̂ — , —— .-—r i r -r -r', i i "T-~r- i i . p i i ' ~ i . i i i i i r-i--,--.- i . i i. i i L i . i,-Li.t-i--t--r-r-T n If) 0

MFTAI FACTOR ^* s 2*50 s 2*o) s i+so s noo s (we s o+oo t EHSO N i+oo H t 1 *50 N ( 2+00 N 2*50 N 3+00 N MF7Al FArjnRFilter * 22 17 69 t. 5 C. 78 1.1 2.8 3. B 2.8 2.5 i. 3 0.94 7 * 1.9 O.W 0.31 0.10 0030 0.030 0.030 0.060 0.18 0.38 0.74 0.91 niter

n*2 1 i "l"" 21s^g ^^^ 3 6 0* 58 0 070 0' M S S ' 3 2 l3 1 l * 1' 5 0' K 1 * 3 ' *'* '' S 0'WO 0'OK O WO 0'0a D' OJO 0' OK 0 -IUO 0' 07I) O l * '" 5 ns^

-1=4 3.* L* 2.5 0.47 1.1 1,3 1.3 /8.7 i. 6 0.89 O.S3 1 2 1.3 1.7 1.5 093 0.050 0.021 0.020 O.OZO O.OW 0.060 0.42 1.2 0.24 0.090 .1=4

,\"\\. - V \

.. ' -X \.- - ' \

•'-' - '"' ^ \RFSI^TIVITV it'* iK505 2'50S 2 tOOS '*50S 1*0)5 ( 0*50 S (MO | 0*50 N UpDN H50 N 2*00 N 2*50 V 3*00 N RfJ^I^TIVITY

Ohm-m Filter.,', "^P" 375^ 475 663 2D30 7405 '* I7B3 1103 1361 1820 2794 317C 1938 11M 1605 7860 121 I8K 21K 23* 26H IX 2* I4K 4951 5132 Rlter Ohm-m

k '. :~'~' J *r - i\M '51^*^ 132. __ 76 . 155 \\x 2B61 , , '5K \ 4W , ,, 1 948 — teTD 1827 1196 1593 — 2W! s 1 MO ^ ^ 324 — . 1448 vNs 1*K 8778 — 7740 — 9031 10K y 19K 25K 25K 21K^ - 3941 0=1 V ^^\( ~ ̂ ^J}\\^((\\\^- -ZZfayf, —— -,\ ~^1 y//— \ ( ,' 1 C——^S~ -*^Z~-^' ^——^.y—— ——— 'y ^ ———— x l ltf/h

'' -•le^S 262 ; 89 f̂ lSt -V" 871 /S SS79 \A 2*3? 4807 iC^ 71S\ 1466 — 1540 1908 5647 2033 (920——1048 1735 \9682 f m . __ W— "T5f^-2!K 3K 351 ) 27IC /J 5761 X 1381 n-2''-^- 7 f̂^'^ \ isx^^^*r Vs- -— — 'V ' y ' P — ^V"\\ ' /^"^ \ s /////-tv ";. . -. ' *Z 3 123^X525'^' 1160 883 v^ 30S7 — 2129 y l 621 __ 768 -~~ 538 —— 1123 ( *976 ^ 3506 1 1434 -* 1 743 -) 1054 1797 \\ 15K ( 25K ^ 39X - 26K 27K \ 32K ^ 24K 'S W& ^ \TS* S 1\\1 0=3' -- //sis-^\ J^\\ /r ^ -̂ . — N\ /" \ f /n 1 'l ^~! ( x' \\\\V\\ /^ ^- __ . v-' //s//// •t-vs/'s'

^ . y. n-4 6W^- 1981 ^ 1049 595 ' N 1937 * 1106 1615^' 355 ' Ki ^- XX 4 IJI ' 2183 — 2270 ' 1553 — 1653 2727 ^ 16K '3* 32K 32K ~— 29K 231 ' ' 5737 7 1689 - 8856 ISH n-4

r r-''

CHARGARIl ITY 5*OOS 2*505 2W S 1+50S 1-KO 5 0^0 S W3D p 5*50 N 1+00 N 1*50 N Z+CO N 2*50 N MO N ( CHARCARII !TY

mV yv filter ^ J5 M 24 23 17 19 29 34 29 Z7 26 K 2B 29 28 1* 10 7.4 8.3 6.8 B.I H 15 20 23 20 Filter mV/V

n-1 ^3 t iv. 48 s + s 25 S 24 v '2 , __ - **// ® J V^*4 ^ l 3 I ^ :J 24 22 r 3 -^31 ,- 28 xV; 7 ' 5J *' 9 *' 8 6 ! 7' 3 7' 5 9' 9 y 1 8 S M nst

0=3 32 26 B '^ 14 X\ 24 (^Jl ^̂ J/ a M /^" 1 ^ ^- 26 27 30 28 25 OO 7.5 6.6 7.2 6.2 S.6 11 y^'9 25. 20 23 n^3

n = 4 23"^ 27 26 *' 2.8^ zT^^-^U^^^ 21 -^31 34 -28 IS M 30 27 26 25 ^* 8.1 8.4 6,7 7.2 11 '19 24 20 ' 2 1 ^ 12 11=4

Line 2850 W

Pole-Dipole Arraya oa a

- — On r®-'nitflr 1 1 i

*"\ x' a s 25.0 M

# * t \ S

* * * * ^9plot point

INTERPRETATION





Scale 1:250025 0 25 50 75 1 00 1 25 1 50

(metres)




DAN PATRIE EXPLORATIONGeosotT 'software for the

geophys rpt on the satterly prop satterly tp...the satterly property is located on birch lake in the...

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